Hon Trung Lon, a granite island off the coast of South Vietnam, is composed solely of a unique, extremely differentiated, high-silica alkali granite of Cretaceous age. An adjacent island, Hon Trung Nho, is composed solely of rhyolitic rock of similar composition. The Hon Trung Nho rhyolite may be a fine-grained equivalent of the granite. Whole-rock potassium-argon analysis suggests that the age of the Hon Trung Lon granite is greater than 70 m.y. and less than 100 m.y. This age implies a previously unrecognized period of intrusion for the zone of granitic rocks outcropping along the northeast side of the Gulf of Thailand. Extensive investigation of the Mesozoic and Tertiary igneous rocks of Southeast Asia, particularly Indochina, including reliable geochronological work, is needed to trace the geologic events that produced the complicated structural features and orogenic history of this region. Existing data suggest that Southeast Asia has been the site of active orogeny since the Paleozoic and that the Hon Trung Lon granite was emplaced through a sialic crust which has been evolving in this area for at least the last 400 m.y.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1967)78[1289:ACATSO]2.0.CO;2","usgsCitation":"Hilde, T.W., and Engel, C.G., 1967, Age, composition, and tectonic setting of the granite island, Hon Trung Lon, off the coast of South Vietnam: Geological Society of America Bulletin, v. 78, no. 10, p. 1289-1294, https://doi.org/10.1130/0016-7606(1967)78[1289:ACATSO]2.0.CO;2.","productDescription":"6 p.","startPage":"1289","endPage":"1294","costCenters":[],"links":[{"id":386423,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Vietnam","otherGeospatial":"south Vietnam Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 106.029052734375,\n 8.407168163601076\n ],\n [\n 106.9573974609375,\n 8.407168163601076\n ],\n [\n 106.9573974609375,\n 8.90678000752024\n ],\n [\n 106.029052734375,\n 8.90678000752024\n ],\n [\n 106.029052734375,\n 8.407168163601076\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"78","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hilde, Thomas W.C.","contributorId":77072,"corporation":false,"usgs":true,"family":"Hilde","given":"Thomas","email":"","middleInitial":"W.C.","affiliations":[],"preferred":false,"id":817421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engel, Celeste G.","contributorId":23386,"corporation":false,"usgs":true,"family":"Engel","given":"Celeste","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":817422,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221357,"text":"70221357 - 1967 - Stratigraphy and correlation of the precambrian belt supergroup of the southern Lewis and Clark Range, Montana","interactions":[],"lastModifiedDate":"2021-06-11T13:11:40.084744","indexId":"70221357","displayToPublicDate":"1967-12-01T08:01:34","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and correlation of the precambrian belt supergroup of the southern Lewis and Clark Range, Montana","docAbstract":"Several well-exposed and little-deformed Belt Supergroup sections have been studied in the southern Lewis and Clark Range. In the area studied, the Belt thins eastward or northeastward due both to primary sedimentation and to pre-Middle Cambrian erosion. These rocks can now be more precisely correlated with the well-known sections near Bonner, Helena, and Glacier National Park. In the western part of the area, the Missoula Group is thickest and lithologically intermediate between the sections at Bonner and Marias Pass. Formation names from these two sections are applied in the southern Lewis and Clark Range. The thin Belt sequence in the eastern part of the area includes the lower part of the Missoula Group and older formations that may be traced southward into the Helena, Empire, and Spokane Formations of the Helena area. Consequently, the Helena Dolomite of the Helena area, the Siyeh Formation of the Marias Pass area, and the \"Newland Limestone\" of the Bonner area are probably lateral equivalents.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1967)78[343:SACOTP]2.0.CO;2","usgsCitation":"McGill, G., and Sommers, D.A., 1967, Stratigraphy and correlation of the precambrian belt supergroup of the southern Lewis and Clark Range, Montana: Geological Society of America Bulletin, v. 78, no. 3, p. 343-352, https://doi.org/10.1130/0016-7606(1967)78[343:SACOTP]2.0.CO;2.","productDescription":"10","startPage":"343","endPage":"352","costCenters":[],"links":[{"id":386419,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Lewis and Clark range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.70898437499999,\n 46.24824991289166\n ],\n [\n -109.654541015625,\n 46.24824991289166\n ],\n [\n -109.654541015625,\n 47.331377157798244\n ],\n [\n -111.70898437499999,\n 47.331377157798244\n ],\n [\n -111.70898437499999,\n 46.24824991289166\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"78","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McGill, G.E.","contributorId":14436,"corporation":false,"usgs":true,"family":"McGill","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":817417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sommers, David A.","contributorId":96761,"corporation":false,"usgs":true,"family":"Sommers","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":817418,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221351,"text":"70221351 - 1967 - Shock effects in certain rock-forming minerals","interactions":[],"lastModifiedDate":"2021-06-11T12:50:31.070123","indexId":"70221351","displayToPublicDate":"1967-12-01T07:46:30","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Shock effects in certain rock-forming minerals","docAbstract":"Shock effects in quartz, plagioclase, biotite, amphibole, and some accessory minerals have been observed in rocks subjected to various degrees of meta morphism by meteoritic impact. The shock features described are unique; they are never observed in rocks from normal geologic environments. Such features are described:
1) Multiple sets of closely spaced planar microstructures occur in quartz, plagioclase, and other rock-forming minerals. Those characteristic of shock consist of alternating platelets, with a range of reduced mean index of re fraction and birefringence; they con sist of platelets that have been partially or completely transformed to an amor phous phase.
2) Quartz and plagioclase are selec tively and completely transformed to silica glass and plagioclase glass in the solid state, whereas the associated mafic minerals remained crystalline. There is no reaction between adjacent minerals.
3) High-pressure polymorphs occur, such as coesite or stishovite. Coesite oc Curs exclusively within silica glass; it has not been observed as a reaction or breakdown product.
4) Nickel-iron spherules occur in the fused glass or impactites.
5) The occurrence of droplets of ilmenite, rutile, pseudobrookite, and baddaleyite in impactites indicates a temperature of formation exceeding 150°C.
6) Dense glass occurs, similar in composition to bulk rock, in which iron oxide, such as fine particles of mag netite, is completely dissolved.
All these features are characteristic of a process involving the rapid rise and fall of extremiiely high pressures and temperatures. Minerals and mineral as semblages experiencing such high strain rates and sudden changes of pressures and temperatures react and change in dependently to the bulk chemical com position, under nonequilibrium condi tions.
Many aspects of shock features re quire careful study. Kink bands in biotite and deformation lamellae in quartz occur in tectonically deformed rocks. These features should be studied with great care in order to determine whether reduction in mean index of refraction and total birefringence along the planar structures have resulted from vitrification or phase transition; their presence is additional evidence in favor of a shock mechanism.
Vitreous phases or glasses formed by shock also have many unique prop erties; they have not been studied by such methods as thermoluminescence, electron spin resonance, low-angle x ray diffraction, or infrared spectroscopy. Shock-fused glass of high density needs to be studied in detail in carefully con trolled laboratory conditions.
Experimental shock-wave studies of the equation-of-state of single minerals and mineral assemblages, under care fully controlled conditions, must pre cede estimates of peak pressures and peak and residual temperatures of shocked natural mineral assemblages. Detailed petrographic and mineralogic studies, however, have provided useful and definitive criteria for characteriza tion of impact events. Such data should be of paramount importance in the study of samples brought back from Moon.
","language":"English","publisher":"AAAS","doi":"10.1126/science.156.3772.192","usgsCitation":"Chao, E.C., 1967, Shock effects in certain rock-forming minerals: Science, v. 156, no. 3772, p. 192-202, https://doi.org/10.1126/science.156.3772.192.","productDescription":"11 p.","startPage":"192","endPage":"202","costCenters":[],"links":[{"id":386413,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"156","issue":"3772","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Chao, E. C. T.","contributorId":96713,"corporation":false,"usgs":true,"family":"Chao","given":"E.","email":"","middleInitial":"C. T.","affiliations":[],"preferred":false,"id":817410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011595,"text":"70011595 - 1967 - Surveyor V: Discussion of chemical analysis","interactions":[],"lastModifiedDate":"2026-02-09T22:12:06.114915","indexId":"70011595","displayToPublicDate":"1967-11-03T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Surveyor V: Discussion of chemical analysis","docAbstract":"Material of basaltic composition at the Surveyor V landing site implies that differentiation has occurred in the moon, probably due to internal sources of heat. The results are consistent with the hypothesis that extensive volcanic flows have been responsible for flooding and filling the mare basins. The processes and products of lunar magmatic activity are apparently similar to those of the earth.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.158.3801.641","usgsCitation":"Gault, D.E., Adams, J.B., Collins, R.J., Green, J., Kuiper, G.P., Mazursky, H., O’Keefe, J.A., Phinney, R.A., and Shoemaker, E., 1967, Surveyor V: Discussion of chemical analysis: Science, v. 158, no. 3801, p. 641-642, https://doi.org/10.1126/science.158.3801.641.","productDescription":"2 p.","startPage":"641","endPage":"642","costCenters":[],"links":[{"id":221680,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Moon","volume":"158","issue":"3801","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba2a3e4b08c986b31f84e","contributors":{"authors":[{"text":"Gault, D. E.","contributorId":38580,"corporation":false,"usgs":true,"family":"Gault","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, J. B.","contributorId":21679,"corporation":false,"usgs":true,"family":"Adams","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":361503,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, R. J.","contributorId":77655,"corporation":false,"usgs":true,"family":"Collins","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":361506,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Green, J.","contributorId":26439,"corporation":false,"usgs":true,"family":"Green","given":"J.","affiliations":[],"preferred":false,"id":361504,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kuiper, G. P.","contributorId":9394,"corporation":false,"usgs":true,"family":"Kuiper","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":361502,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mazursky, H.","contributorId":7417,"corporation":false,"usgs":true,"family":"Mazursky","given":"H.","email":"","affiliations":[],"preferred":false,"id":361500,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"O’Keefe, J. A.","contributorId":92420,"corporation":false,"usgs":true,"family":"O’Keefe","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361508,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Phinney, R. A.","contributorId":8609,"corporation":false,"usgs":true,"family":"Phinney","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361501,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Shoemaker, E.M.","contributorId":81499,"corporation":false,"usgs":true,"family":"Shoemaker","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":361507,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70010486,"text":"70010486 - 1967 - Surveyor V: Television pictures","interactions":[],"lastModifiedDate":"2026-02-09T22:14:58.172744","indexId":"70010486","displayToPublicDate":"1967-11-03T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Surveyor V: Television pictures","docAbstract":"Surveyor V landed in a small crater, 8.5 meters wide and 12.5 meters long, which was probably formed by drainage of surficial fragmental debris into a subsurface fissure. The lunar surface debris layer is exposed in the walls of this crater. At depths below about 10 centimeters, the debris appears to be composed mainly of shock-compressed aggregates, ranging from a few millimeters up to 3 centimeters in diameter, set in a matrix of less-coherent finer particles. Rocky chips and fragments larger than a millimeter are dispersed as a subordinate constituent of the debris.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.158.3801.642","issn":"00368075","usgsCitation":"Shoemaker, E., Batson, R.M., Holt, H.E., Morris, E.C., Rennilson, J.J., and Whitaker, E.A., 1967, Surveyor V: Television pictures: Science, v. 158, no. 3801, p. 642-652, https://doi.org/10.1126/science.158.3801.642.","productDescription":"11 p.","startPage":"642","endPage":"652","costCenters":[],"links":[{"id":219241,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Moon","volume":"158","issue":"3801","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba2a4e4b08c986b31f857","contributors":{"authors":[{"text":"Shoemaker, E.M.","contributorId":81499,"corporation":false,"usgs":true,"family":"Shoemaker","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":359037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batson, R. M.","contributorId":76714,"corporation":false,"usgs":true,"family":"Batson","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":359036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holt, H. E.","contributorId":64694,"corporation":false,"usgs":true,"family":"Holt","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359035,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morris, E. C.","contributorId":84381,"corporation":false,"usgs":true,"family":"Morris","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359038,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rennilson, J. J.","contributorId":107336,"corporation":false,"usgs":true,"family":"Rennilson","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359039,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Whitaker, E. A.","contributorId":43086,"corporation":false,"usgs":true,"family":"Whitaker","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359034,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70210848,"text":"70210848 - 1967 - Ancient geomagnetic field intensities—II geological data: Sets G1–G21 historic and archeological data: H10–H13","interactions":[],"lastModifiedDate":"2020-06-30T12:04:25.202407","indexId":"70210848","displayToPublicDate":"1967-11-01T11:33:24","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Ancient geomagnetic field intensities—II geological data: Sets G1–G21 historic and archeological data: H10–H13","docAbstract":"No abstract available.
","language":"English","publisher":"Oxford Academic","doi":"10.1111/j.1365-246X.1967.tb02300.x","usgsCitation":"Smith, P.J., 1967, Ancient geomagnetic field intensities—II geological data: Sets G1–G21 historic and archeological data: H10–H13: Geophysical Journal International, v. 13, no. 5, p. 483-486, https://doi.org/10.1111/j.1365-246X.1967.tb02300.x.","productDescription":"4 p.","startPage":"483","endPage":"486","costCenters":[],"links":[{"id":480341,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.1967.tb02300.x","text":"Publisher Index Page"},{"id":375983,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, Peter J.","contributorId":225580,"corporation":false,"usgs":false,"family":"Smith","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":791703,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70210847,"text":"70210847 - 1967 - Viscosity and finite strength of the mantle as determined from water and ice loads","interactions":[],"lastModifiedDate":"2020-06-29T16:18:51.948045","indexId":"70210847","displayToPublicDate":"1967-11-01T11:07:12","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Viscosity and finite strength of the mantle as determined from water and ice loads","docAbstract":"Some recent examples of transient Earth loads (Lake Bonneville, Utah; Glacier Bay, Alaska; northeast Greenland) indicate that both the viscosity and finite strength of the mantle are lower than is commonly presumed. A time constant (1/e) of 4000 years is estimated for Lake Bonneville, and of 1000 years for northeast Greenland. A strain rate of 10−14 is typical. These figures imply viscosities in a homogeneous half space ranging from 1020 to 1021 poises.
An upper limit of finite strength is set by Lake Bonneville at a few times 106 dyn/cm2. If mountain ranges like the Sierra Nevada or Himalaya are regarded as dynamically supported rather than static systems, this low value is not incompatible with other geologic observations.
","language":"English","publisher":"Oxford Academic","doi":"10.1111/j.1365-246X.1967.tb06243.x","usgsCitation":"Crittenden, M.D., 1967, Viscosity and finite strength of the mantle as determined from water and ice loads: Geophysical Journal International, v. 14, no. 1-4, p. 261-279, https://doi.org/10.1111/j.1365-246X.1967.tb06243.x.","productDescription":"19 p.","startPage":"261","endPage":"279","costCenters":[],"links":[{"id":480342,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.1967.tb06243.x","text":"Publisher Index Page"},{"id":375982,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Greenland, United States","state":"Alaska, Utah","otherGeospatial":"Glacier Bay, Lake Bonneville, Mesters Vig","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -24.5159912109375,\n 71.99003064007077\n ],\n [\n -23.52996826171875,\n 71.99003064007077\n ],\n [\n -23.52996826171875,\n 72.36577662200845\n ],\n [\n -24.5159912109375,\n 72.36577662200845\n ],\n [\n -24.5159912109375,\n 71.99003064007077\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -135.087890625,\n 59.567723306212955\n ],\n [\n -137.691650390625,\n 58.802361927759456\n ],\n [\n -136.0546875,\n 57.54531289147553\n ],\n [\n -134.80224609375,\n 56.19448087726972\n ],\n [\n -132.37426757812497,\n 57.00485033534416\n ],\n [\n -133.59375,\n 58.45348121776238\n ],\n [\n -135.087890625,\n 59.361195471124816\n ],\n [\n -135.087890625,\n 59.567723306212955\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.3896484375,\n 39.13006024213511\n ],\n [\n -111.39038085937499,\n 39.13006024213511\n ],\n [\n -111.39038085937499,\n 43.04480541304369\n ],\n [\n -114.3896484375,\n 43.04480541304369\n ],\n [\n -114.3896484375,\n 39.13006024213511\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"14","issue":"1-4","noUsgsAuthors":false,"publicationDate":"2010-01-26","publicationStatus":"PW","contributors":{"authors":[{"text":"Crittenden, Max D. Jr.","contributorId":28951,"corporation":false,"usgs":true,"family":"Crittenden","given":"Max","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":791702,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221362,"text":"70221362 - 1967 - Oligocene or younger thrust faulting in the Ruby Mountains, northeastern Nevada","interactions":[],"lastModifiedDate":"2021-06-11T13:43:01.17514","indexId":"70221362","displayToPublicDate":"1967-11-01T08:37:38","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Oligocene or younger thrust faulting in the Ruby Mountains, northeastern Nevada","docAbstract":"A klippe of unmetamorphosed Devonian carbonate rocks rests on the Harrison Pass intrusive body south of Toyn Creek in the central Ruby Mountains, Elko County, Nevada. This klippe and other klippen of Carboniferous strata - first mapped by R. P. Sharp (1942) - that rest on lower Paleozoic strata are believed to represent a once-continuous thrust sheet that developed after emplacement of the intrusive body. This intrusion of coarse-grained granodiorite to quartz monzonite is exposed over an area of about 45 square miles. Potassium-argon and lead-alpha age determinations on four samples of the intrusive body establish Oligocene or younger age for the thrusting. Potassium-argon age determinations on biotites from the four samples range from 29 to 36 m.y. with a possible analytical error of ±10 percent. Lead-alpha age determinations (all with a possible analytical error of ±10 m.y.) on zircon showed 40 m.y. for three of the samples and 30 m.y. for the fourth. Lead-alpha and potassium-argon dates on a fifth sample collected by R. R. Coats also fall within these ranges. The agreement of the radiometric dates indicates a lack of thermal activity subsequent to the emplacement of the intrusion and establishes a maximum age of Oligocene for the thrust faulting. The present distribution of thermally metamorphosed Paleozoic rocks in the Ruby Mountains seems to preclude the possibility that the thrust plate originated within the Ruby Mountains. Sharp suggested a western source with displacement of from 7 to 10 miles.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1967)78[1345:OOYTFI]2.0.CO;2","usgsCitation":"Willden, R., Hermann, T.A., and Stern, T., 1967, Oligocene or younger thrust faulting in the Ruby Mountains, northeastern Nevada: Geological Society of America Bulletin, v. 78, no. 11, p. 1345-1358, https://doi.org/10.1130/0016-7606(1967)78[1345:OOYTFI]2.0.CO;2.","productDescription":"14 p.","startPage":"1345","endPage":"1358","costCenters":[],"links":[{"id":386425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"northern Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.981689453125,\n 39.83385008019448\n ],\n [\n -114.04907226562499,\n 39.83385008019448\n ],\n [\n -114.04907226562499,\n 42.00032514831621\n ],\n [\n -119.981689453125,\n 42.00032514831621\n ],\n [\n -119.981689453125,\n 39.83385008019448\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"78","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Willden, Ronald","contributorId":107368,"corporation":false,"usgs":true,"family":"Willden","given":"Ronald","affiliations":[],"preferred":false,"id":817425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hermann, Thomas A. thomas_hermann@usgs.gov","contributorId":5210,"corporation":false,"usgs":true,"family":"Hermann","given":"Thomas","email":"thomas_hermann@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":817426,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stern, T.W.","contributorId":258270,"corporation":false,"usgs":false,"family":"Stern","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":817427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70227054,"text":"70227054 - 1967 - Chapter III: Television observations from Surveyor V","interactions":[],"lastModifiedDate":"2021-12-28T15:37:08.972575","indexId":"70227054","displayToPublicDate":"1967-11-01T08:18:44","publicationYear":"1967","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"displayTitle":"Chapter III: Television observations from Surveyor V","title":"Chapter III: Television observations from Surveyor V","docAbstract":"Surveyor V landed on the lunar surface at 00:46:44 GMT on Day 254 (September 11), 35 hr after local sunrise on the moon. Between the time of landing and lunar sunset, 13 days later, it transmitted more than 18,000 high-quality television pictures of the lunar surface and parts of the spacecraft. The Surveyor V camera was operated extensively from the Goldstone, California, and Canberra, Australia, Tracking Stations of the Deep Space Network; some pictures were also received at the Madrid, Spain, Tracking Station.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Surveyor V mission report: Part II: Science results","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Jet Propulsion Laboratory","usgsCitation":"Shoemaker, E.M., Batson, R.M., Holt, H.E., Morris, E.C., Rennilson, J.J., and Whitaker, E.A., 1967, Chapter III: Television observations from Surveyor V, chap. of Surveyor V mission report: Part II: Science results, p. 7-42.","productDescription":"JPL TR-32-1246, 36 p.","startPage":"7","endPage":"42","costCenters":[],"links":[{"id":393497,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":393495,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ntrs.nasa.gov/api/citations/19680003577/downloads/19680003577.pdf","size":"14.3 MB","linkFileType":{"id":1,"text":"pdf"}}],"otherGeospatial":"Mare Tranquillitatis, Moon, Theophilus crater","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":829403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batson, R. M.","contributorId":76714,"corporation":false,"usgs":true,"family":"Batson","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":829404,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holt, H. E.","contributorId":64694,"corporation":false,"usgs":true,"family":"Holt","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":829405,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morris, E. C.","contributorId":84381,"corporation":false,"usgs":true,"family":"Morris","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":829406,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rennilson, J. J.","contributorId":107336,"corporation":false,"usgs":true,"family":"Rennilson","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":829407,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Whitaker, E. A.","contributorId":43086,"corporation":false,"usgs":true,"family":"Whitaker","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":829408,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":1001583,"text":"1001583 - 1967 - Back-pack unit for capturing waterfowl and upland game by night-lighting","interactions":[],"lastModifiedDate":"2025-02-12T15:45:45.248481","indexId":"1001583","displayToPublicDate":"1967-10-06T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Back-pack unit for capturing waterfowl and upland game by night-lighting","docAbstract":"A night-lighting unit, designed as a light weight back-pack, proved successful for capturing waterfowl pairs, pheasants (Phasianus colchicus), and cottontail rabbits (Sylvilagus floridanus) during the spring and summer when most breeding populations are widely dispersed. Eighty ducks of seven species were captured in 48 hours (1.7 ducks per hour) of night-lighting in marsh habitat. Similarly, 30 pheasants were trapped in 25 hours (1.2 birds per hour) and 63 cottontail rabbits were either observed at close range (6-12 ft) or captured during night-lighting operations in upland habitat. Catch per hour of effort increased for all species as their night habitat requirements and reaction to night-lights became known. The mobile unit proved well suited for intensive use on small areas where other methods of capture were unfeasible and where representative coverage of various habitat types was desired. Besides its utility for capturing animals, the unit provided a method for studying nocturnal movements, behavior, and habitat use of marked animals.
","language":"English","publisher":"Wiley","doi":"10.2307/3797983","usgsCitation":"Drewien, R., Reeves, H., Springer, P.F., and Kuck, T., 1967, Back-pack unit for capturing waterfowl and upland game by night-lighting: Journal of Wildlife Management, v. 31, no. 4, p. 778-783, https://doi.org/10.2307/3797983.","productDescription":"6 p.","startPage":"778","endPage":"783","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133766,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Day County, Sanborn County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-97.9802,45.5883],[-97.6116,45.5882],[-97.4885,45.5892],[-97.3727,45.5889],[-97.3629,45.5603],[-97.3544,45.5605],[-97.2269,45.5603],[-97.226,45.2996],[-97.2251,45.2118],[-97.226,45.1538],[-97.2396,45.1541],[-97.4951,45.1537],[-97.7403,45.1544],[-97.9809,45.1545],[-97.9803,45.2409],[-97.9802,45.5883]]],[[[-97.8506,44.1964],[-97.8494,43.8505],[-97.9662,43.851],[-98.3266,43.851],[-98.331,43.8502],[-98.332,43.9385],[-98.332,44.1974],[-97.8506,44.1964]]]]},\"properties\":{\"name\":\"Day\",\"state\":\"SD\"}}]}","volume":"31","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adb9","contributors":{"authors":[{"text":"Drewien, Rod C.","contributorId":58594,"corporation":false,"usgs":true,"family":"Drewien","given":"Rod C.","affiliations":[],"preferred":false,"id":311299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, H.M.","contributorId":92634,"corporation":false,"usgs":true,"family":"Reeves","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":311300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Springer, P. F.","contributorId":56590,"corporation":false,"usgs":false,"family":"Springer","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":311298,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kuck, T.L.","contributorId":101591,"corporation":false,"usgs":true,"family":"Kuck","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":311301,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70205789,"text":"70205789 - 1967 - Salt resources of Thailand","interactions":[],"lastModifiedDate":"2019-10-03T11:37:29","indexId":"70205789","displayToPublicDate":"1967-10-03T11:33:49","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5868,"text":"Report of Investigation - Thailand, Department of Mineral Resources","printIssn":" 0563-353","active":false,"publicationSubtype":{"id":10}},"title":"Salt resources of Thailand","docAbstract":"In recent years beds of rock salt, as much as 820 feet thick, have been found in the subsurface of northeastern Thailand in a thick sequence of 'red beds' of the Maha Sarakam formation at the top of the Korat group of Mesozoic age. These salt-bearing rocks are widespread in the subsurface of northeastern Thailand and extend under the Mekong river into Laos to form one of the major salt-bearing regions of the world. The Korat group was deposited during Triassic, Jurassic and Cretaceous times on floodplains and in shallow estuaries, bays, or partly isolated coastal lakes over a large arid or semiarid region that lay near sea level and sank very slowly under remarkably uniform conditions. Total reserves are estimated at more than 2,700 billion tons of inferred rock salt in seven areas or deposits that include only about 20 percent of the total area of about 40,000 square kilometers probably underlain by salt-bearing rocks.
","language":"English","publisher":"Thailand Department of Mineral Resources","publisherLocation":"Bangkok, Thailand","issn":"0563-3532","usgsCitation":"Gardner, L.S., 1967, Salt resources of Thailand: Report of Investigation - Thailand, Department of Mineral Resources, v. 11, 100 p.","productDescription":"100 p.","costCenters":[],"links":[{"id":367963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Thailand","otherGeospatial":"Northeastern Thailand","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[102.58493,12.18659],[101.68716,12.64574],[100.83181,12.62708],[100.97847,13.41272],[100.0978,13.40686],[100.01873,12.307],[99.47892,10.84637],[99.15377,9.96306],[99.2224,9.23926],[99.87383,9.20786],[100.27965,8.29515],[100.45927,7.42957],[101.01733,6.85687],[101.62308,6.74062],[102.14119,6.22164],[101.81428,5.81081],[101.15422,5.69138],[101.07552,6.20487],[100.2596,6.64282],[100.08576,6.46449],[99.69069,6.84821],[99.51964,7.34345],[98.98825,7.90799],[98.50379,8.38231],[98.33966,7.79451],[98.15001,8.35001],[98.25915,8.97392],[98.55355,9.93296],[99.03812,10.96055],[99.58729,11.89276],[99.19635,12.80475],[99.21201,13.26929],[99.09776,13.8275],[98.43082,14.62203],[98.19207,15.1237],[98.53738,15.3085],[98.90335,16.17782],[98.49376,16.83784],[97.85912,17.56795],[97.3759,18.44544],[97.79778,18.62708],[98.25372,19.7082],[98.95968,19.75298],[99.54331,20.1866],[100.11599,20.41785],[100.54888,20.10924],[100.60629,19.50834],[101.28201,19.46258],[101.03593,18.40893],[101.05955,17.5125],[102.11359,18.1091],[102.413,17.93278],[102.99871,17.96169],[103.20019,18.30963],[103.95648,18.24095],[104.71695,17.42886],[104.77932,16.44186],[105.58904,15.57032],[105.54434,14.72393],[105.21878,14.27321],[104.28142,14.41674],[102.98842,14.22572],[102.3481,13.39425],[102.58493,12.18659]]]},\"properties\":{\"name\":\"Thailand\"}}]}","volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gardner, Louis S.","contributorId":81581,"corporation":false,"usgs":true,"family":"Gardner","given":"Louis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":772354,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70205787,"text":"70205787 - 1967 - Phichit gypsum deposit, central Thailand","interactions":[],"lastModifiedDate":"2019-10-03T11:28:10","indexId":"70205787","displayToPublicDate":"1967-10-03T10:53:06","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5868,"text":"Report of Investigation - Thailand, Department of Mineral Resources","printIssn":" 0563-353","active":false,"publicationSubtype":{"id":10}},"title":"Phichit gypsum deposit, central Thailand","docAbstract":"An extensive deposit of white, granular, massive gypsum has been discovered in central Thailand. The gypsum, a part of the Mesozoic Korat group, was deposited along with salt by evaporation of sea water in shallow basins extensively developed in Thailand and adjacent parts of Laos. It now occurs in a narrow, deep downfaulted block enclosed within a complex of Paleozoic sedimentary rocks and younger volcanic rocks, and is bounded to the east and west by north-trending high-angle faults. During downfaulting to its present position, the gypsum was altered to anhydrite. The upper part of the deposit has been reconverted to gypsum during the present cycle of erosion to depths of about 80-120 feet. Total reserves may exceed 25 million tons of gypsum with perhaps 10 times as much anhydrite.
","language":"English","publisher":"Thailand Department of Mineral Resources","issn":"0563-3532","usgsCitation":"Gardner, L.S., 1967, Phichit gypsum deposit, central Thailand: Report of Investigation - Thailand, Department of Mineral Resources, v. 9, 42 p.","productDescription":"42 p.","costCenters":[],"links":[{"id":367960,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Thailand","otherGeospatial":"Central Thailand","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[102.58493,12.18659],[101.68716,12.64574],[100.83181,12.62708],[100.97847,13.41272],[100.0978,13.40686],[100.01873,12.307],[99.47892,10.84637],[99.15377,9.96306],[99.2224,9.23926],[99.87383,9.20786],[100.27965,8.29515],[100.45927,7.42957],[101.01733,6.85687],[101.62308,6.74062],[102.14119,6.22164],[101.81428,5.81081],[101.15422,5.69138],[101.07552,6.20487],[100.2596,6.64282],[100.08576,6.46449],[99.69069,6.84821],[99.51964,7.34345],[98.98825,7.90799],[98.50379,8.38231],[98.33966,7.79451],[98.15001,8.35001],[98.25915,8.97392],[98.55355,9.93296],[99.03812,10.96055],[99.58729,11.89276],[99.19635,12.80475],[99.21201,13.26929],[99.09776,13.8275],[98.43082,14.62203],[98.19207,15.1237],[98.53738,15.3085],[98.90335,16.17782],[98.49376,16.83784],[97.85912,17.56795],[97.3759,18.44544],[97.79778,18.62708],[98.25372,19.7082],[98.95968,19.75298],[99.54331,20.1866],[100.11599,20.41785],[100.54888,20.10924],[100.60629,19.50834],[101.28201,19.46258],[101.03593,18.40893],[101.05955,17.5125],[102.11359,18.1091],[102.413,17.93278],[102.99871,17.96169],[103.20019,18.30963],[103.95648,18.24095],[104.71695,17.42886],[104.77932,16.44186],[105.58904,15.57032],[105.54434,14.72393],[105.21878,14.27321],[104.28142,14.41674],[102.98842,14.22572],[102.3481,13.39425],[102.58493,12.18659]]]},\"properties\":{\"name\":\"Thailand\"}}]}","volume":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gardner, Louis S.","contributorId":81581,"corporation":false,"usgs":true,"family":"Gardner","given":"Louis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":772343,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221319,"text":"70221319 - 1967 - Demountable hot hollow cathode lamp as excitation source in atomic fluorescence flame spectrometry","interactions":[],"lastModifiedDate":"2021-06-09T18:56:02.438198","indexId":"70221319","displayToPublicDate":"1967-10-01T13:49:16","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Demountable hot hollow cathode lamp as excitation source in atomic fluorescence flame spectrometry","docAbstract":"No abstract available.
","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac60256a018","usgsCitation":"Dinnin, J., and Helzer, C.J., 1967, Demountable hot hollow cathode lamp as excitation source in atomic fluorescence flame spectrometry: Analytical Chemistry, v. 39, no. 12, p. 1489-1491, https://doi.org/10.1021/ac60256a018.","productDescription":"3 p.","startPage":"1489","endPage":"1491","costCenters":[],"links":[{"id":386365,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"12","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Dinnin, J. I.","contributorId":50886,"corporation":false,"usgs":true,"family":"Dinnin","given":"J. I.","affiliations":[],"preferred":false,"id":817296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helzer, Christopher J.","contributorId":41724,"corporation":false,"usgs":true,"family":"Helzer","given":"Christopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":817297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221318,"text":"70221318 - 1967 - Atomic fluorescence flame spectrometric detection of palladium, titanium, zirconium, chromium, and aluminum using a hot hollow cathode lamp","interactions":[],"lastModifiedDate":"2021-06-09T18:48:20.753747","indexId":"70221318","displayToPublicDate":"1967-10-01T13:43:46","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Atomic fluorescence flame spectrometric detection of palladium, titanium, zirconium, chromium, and aluminum using a hot hollow cathode lamp","docAbstract":"No abstract available.
","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac60256a019","usgsCitation":"Dinnin, J.I., 1967, Atomic fluorescence flame spectrometric detection of palladium, titanium, zirconium, chromium, and aluminum using a hot hollow cathode lamp: Analytical Chemistry, v. 39, no. 12, p. 1491-1493, https://doi.org/10.1021/ac60256a019.","productDescription":"3 p.","startPage":"1491","endPage":"1493","costCenters":[],"links":[{"id":386364,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"12","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Dinnin, Joseph Isadore","contributorId":47842,"corporation":false,"usgs":true,"family":"Dinnin","given":"Joseph","email":"","middleInitial":"Isadore","affiliations":[],"preferred":false,"id":817295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221316,"text":"70221316 - 1967 - Test hold in aquifer with many water-bearing zones at Jacksonville, Florida","interactions":[],"lastModifiedDate":"2021-06-09T18:35:59.361297","indexId":"70221316","displayToPublicDate":"1967-10-01T13:30:27","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Test hold in aquifer with many water-bearing zones at Jacksonville, Florida","docAbstract":"One of the deepest water‐exploration wells in the southeastern United States was completed in 1966 at Jacksonville, Florida. It was drilled to a depth of nearly 2,500 feet to supply geologic and hydrologic information on the deeper unexplored part of the Floridan aquifer. This aquifer consists of a series of water producing zones separated by nonproducing zones. An important new fresh‐water producing zone was found, and the contact between the fresh water and salt water was located. The well was completed in three separate zones so that it could be used to monitor the the deeper part of the aquifer to detect any salt‐water encroachment. This paper describes the objectives, techniques, and results of drilling the test well.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01621.x","usgsCitation":"Leve, G., and Goolsby, D.A., 1967, Test hold in aquifer with many water-bearing zones at Jacksonville, Florida: Groundwater, v. 5, no. 4, p. 18-22, https://doi.org/10.1111/j.1745-6584.1967.tb01621.x.","productDescription":"5 p.","startPage":"18","endPage":"22","costCenters":[],"links":[{"id":386362,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","city":"Jacksonville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.1337890625,\n 30.088107753367257\n ],\n [\n -81.2109375,\n 30.088107753367257\n ],\n [\n -81.2109375,\n 30.543338954230222\n ],\n [\n -82.1337890625,\n 30.543338954230222\n ],\n [\n -82.1337890625,\n 30.088107753367257\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Leve, G.W.","contributorId":64294,"corporation":false,"usgs":true,"family":"Leve","given":"G.W.","affiliations":[],"preferred":false,"id":817292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":817293,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221313,"text":"70221313 - 1967 - New approaches to water‐resources investigations in upstate New York","interactions":[],"lastModifiedDate":"2021-06-09T18:00:54.224471","indexId":"70221313","displayToPublicDate":"1967-10-01T12:55:53","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"New approaches to water‐resources investigations in upstate New York","docAbstract":"The scope of area1 investigations of water resources in New York has changed within the last 4 years. Prior 1962, most investigations covered only counties or smaller areas and were mainly restricted to ground‐water resources Since 1762, investigarions have covered largebasin (2,000‐4,000 square miles) with the purpose of defining total water resources so that basin‐wldc comprehensive plans for water development can be prepared. Ground water has been intensively studied in the basin investigations, both because of its large potential for future development, and becaus e of it sinterre lation with the surface‐water resources. The latter reason is particularly important because the principal aquifers are numerous u nconnect edglacials and andgravel deposits that are crossed by streams. This ground‐water regimen to a large degree determines the flow characteristics and water quality of streams. Conversely, streamflow data provide acon‐venient means of assessing ground‐water availability.Some approaches used in basin studies are: (1)(1) numerous quantitative and qualitative observations of low streamflow to define the principal areas of ground‐water discharge and to define the quantity and quality of discharging ground water (2)estimation of total ground‐water dischar gepas stream gages from daily streamflow records by correlation with ground‐water levels and by analysis of the records (3) assessment of recharge to particular sand and gravel deposit swith inbroadlimits, using the data on ground‐water discharge to streams (4) estimation of a daily chemical quality hydrograph on the basis of quantity and quality of both ground‐water discharge and overland runoff.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01619.x","usgsCitation":"La Sala, A.M., 1967, New approaches to water‐resources investigations in upstate New York: Groundwater, v. 5, no. 4, p. 6-11, https://doi.org/10.1111/j.1745-6584.1967.tb01619.x.","productDescription":"6 p.","startPage":"6","endPage":"11","costCenters":[],"links":[{"id":386359,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"upstate New York","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.32202148437499,\n 42.97250158602597\n ],\n [\n -73.070068359375,\n 42.97250158602597\n ],\n [\n -73.070068359375,\n 45.01141864227728\n ],\n [\n -76.32202148437499,\n 45.01141864227728\n ],\n [\n -76.32202148437499,\n 42.97250158602597\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"La Sala, A. M. Jr.","contributorId":38199,"corporation":false,"usgs":true,"family":"La Sala","given":"A.","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":817289,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5221274,"text":"5221274 - 1967 - The ineffectiveness of acid-fast inclusions in diagnosis of lead poisoning in Canada geese","interactions":[],"lastModifiedDate":"2025-12-15T16:16:19.984578","indexId":"5221274","displayToPublicDate":"1967-10-01T12:17:36","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1140,"text":"Bulletin of the Wildlife Disease Association","active":true,"publicationSubtype":{"id":10}},"title":"The ineffectiveness of acid-fast inclusions in diagnosis of lead poisoning in Canada geese","docAbstract":"No abstract available.
","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-3.4.176","usgsCitation":"Locke, L.N., Bagley, G.E., and Young, L.T., 1967, The ineffectiveness of acid-fast inclusions in diagnosis of lead poisoning in Canada geese: Bulletin of the Wildlife Disease Association, v. 3, no. 4, https://doi.org/10.7589/0090-3558-3.4.176.","productDescription":"1 p.","startPage":"176","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193930,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d7e0","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":333462,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bagley, George E.","contributorId":46589,"corporation":false,"usgs":true,"family":"Bagley","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":333461,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Young, L. T.","contributorId":76420,"corporation":false,"usgs":true,"family":"Young","given":"L.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":333463,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000180,"text":"1000180 - 1967 - Some oligochaetes from Lake Michigan","interactions":[],"lastModifiedDate":"2026-03-12T15:26:52.872993","indexId":"1000180","displayToPublicDate":"1967-10-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3625,"text":"Transactions of the American Microscopical Society","active":true,"publicationSubtype":{"id":10}},"title":"Some oligochaetes from Lake Michigan","docAbstract":"Twenty-six species of Tubificidae, 12 Naididae, and 1 Lumbriculidae were found in three regions of Lake Michigan- Green Bay, the southern end of the lake proper, and the harbor at Ludington, Michigan. One new naidid species is described. Methods of identification of some species are discussed and illustrated. The abundance of oligochaetes and distribution of certain species vary with depth and location. Data are presented on the effects of the environment on the distribution of certain species. The presence or absence of some species reflected the quality of the environment; some were prevalent in polluted waters whereas others were restricted or absent. Possible changes in composition and abundance of species are outlined if organic enrichment increases in Lake Michigan.
","language":"English","publisher":"Wiley","doi":"10.2307/3224267","usgsCitation":"Hiltunen, J.K., 1967, Some oligochaetes from Lake Michigan: Transactions of the American Microscopical Society, v. 86, no. 4, p. 433-454, https://doi.org/10.2307/3224267.","productDescription":"22 p.","startPage":"433","endPage":"454","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130511,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois, Indiana, Michigan, Wisconsin","otherGeospatial":"Lake Michigan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -87.97025984791705,\n 45.20587410008886\n ],\n [\n -88.14054252464355,\n 41.50726553497216\n ],\n [\n -86.33381625694446,\n 41.50940165221235\n ],\n [\n -85.83636960569008,\n 44.47722673256698\n ],\n [\n -85.09881343279604,\n 44.956609541015666\n ],\n [\n -84.6020024557969,\n 45.768004056882816\n ],\n [\n -84.97649940103136,\n 46.22260358684156\n ],\n [\n -86.6882000784625,\n 46.0039491403779\n ],\n [\n -87.97025984791705,\n 45.20587410008886\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"86","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8f3f","contributors":{"authors":[{"text":"Hiltunen, Jarl K.","contributorId":27820,"corporation":false,"usgs":true,"family":"Hiltunen","given":"Jarl","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":308199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003268,"text":"1003268 - 1967 - Clearance and registration of chemical tools for fisheries","interactions":[],"lastModifiedDate":"2025-08-04T15:35:28.444941","indexId":"1003268","displayToPublicDate":"1967-10-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Clearance and registration of chemical tools for fisheries","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8640(1967)29[187:CAROCT]2.0.CO;2","usgsCitation":"Lennon, R.E., 1967, Clearance and registration of chemical tools for fisheries: Progressive Fish-Culturist, v. 29, no. 4, p. 187-193, https://doi.org/10.1577/1548-8640(1967)29[187:CAROCT]2.0.CO;2.","productDescription":"7 p.","startPage":"187","endPage":"193","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131430,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672af2","contributors":{"authors":[{"text":"Lennon, Robert E.","contributorId":14341,"corporation":false,"usgs":true,"family":"Lennon","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":313045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206898,"text":"70206898 - 1967 - Chemical Composition of Ectoprocta (Bryozoa)","interactions":[],"lastModifiedDate":"2019-11-26T11:00:51","indexId":"70206898","displayToPublicDate":"1967-09-30T10:57:18","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"Chemical Composition of Ectoprocta (Bryozoa)","docAbstract":"Published data on the elemental composition of the Ectoprocta (Bryozoa) are supplemented by new chemical analyses of 28 ectoproct samples, distributed among 13 species, for organic matter, CO2 calcium, magnesium, strontium, barium, phosphorus and iron. The new data, in addition to the 25 fairly complete analyses previously published (distributed among 19 other species) suggest the existence of 3 species groupings that are based on composition and are related to habitat. Group I consists of genera that have more than 50 percent organic matter (dry weight). It includes all species of the entirely freshwater Phylactolaemata and the commonly brackish-water and freshwater Ctenostomata. Group II includes Cheilostomata having from 25 to 50 percent organic matter (dry weight). These genera are bush-like in growth habit and may be anchored to fine-grained sediment bottoms. Genera in Group II contain appreciable amounts of P2O5 (1.0-2.0 percent) and Fe2O3 (0.4-1.0 percent) in the ash. Only calcite has been observed in the mineralized portion of the skeleton of Group II species. Group III includes Cheilostomata and Cyclostomata that have less than 25 percent organic matter. These forms require stable surfaces for colonization. They contain a lesser amount of P2O5 (0.1-0.6 percent) and of Fe2O3 (less than 0.4 percent) than Group II genera. About 15 percent of Group III species have aragonitic skeletons. \"Pure\" aragonitic hard parts contain about 1.0 percent SrO (1.4 wt. percent SrCO3 and 0.3 percent MgO (0.6 wt. percent MgCO3) whereas \"pure\" calcitic skeletons contain less than 0.4 percent SrO (0.6 wt. percent SrCO3) and more than 3.5 percent MgO (7.4 wt. percent MgCO3). Based on the few species analyzed, some additional taxonomic and ecologic generalizations are suggested. Calcitic cheilostomes contain more magnesium than do calcitic cyclostomes. Warm water calcitic species have higher magnesium concentrations than do cold water calcitic species. Specimens from an estuary contain more P2O5 and less strontium than do specimens from areas of normal marine salinity, and specimens from nearshore areas have more iron than do specimens from deeper offshore areas. The order of concentration of elements in ectoprocts relative to the composition of sea water is 105 for phosphorus and iron, 103 for barium, 102 for calcium and strontium, and 101 for magnesium. However, the elements that are highly enriched in ectoprocts, especially iron and phosphorus, may be supplied to a considerable extent by sources other than normal sea water, such as food (diatoms in particular), and occluded matter of terrigenous origin. Twenty-eight protein and chitin amino acids were studied in three representative marine ectoproct species: Bugula simplex, a calcitic cheilostome, Parasmittina nitida, an aragonitic cheilostome, and Tubulipora liliacea, a calcitic cyclostome. Similar proportions but widely different amounts (from 0.6 to 11 percent organism dry weight) of amino acids occur in these species. Obvious variations in amino acid proportions relate more directly to degree of calcification and to mineralogy than to species classification. Chitin amino acids recoverable in residues after leaching with acid form less than 2 percent of the total organic content of the organism.
","language":"English","publisher":"SEPM Society for Sedimentary Geology","usgsCitation":"Schopf, T., and Manheim, F.T., 1967, Chemical Composition of Ectoprocta (Bryozoa): Journal of Paleontology, v. 41, no. 5, p. 1197-1225.","productDescription":"29 p.","startPage":"1197","endPage":"1225","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":369636,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":369635,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/1302092"}],"volume":"41","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schopf, T.J.M.","contributorId":106754,"corporation":false,"usgs":true,"family":"Schopf","given":"T.J.M.","email":"","affiliations":[],"preferred":false,"id":776187,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":776188,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70205374,"text":"70205374 - 1967 - Compilation of surface water records of Nepal through December 31, 1965","interactions":[],"lastModifiedDate":"2019-09-16T12:28:36","indexId":"70205374","displayToPublicDate":"1967-09-17T12:23:55","publicationYear":"1967","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Compilation of surface water records of Nepal through December 31, 1965","docAbstract":"No Abstract available
","language":"English","publisher":"Kathmandu H.S.D.","usgsCitation":" Nepal Hydrological Survey Department., 1967, Compilation of surface water records of Nepal through December 31, 1965, 66 p.","productDescription":"66 p.","numberOfPages":"66","costCenters":[],"links":[{"id":367437,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://202.45.147.158/cgi-bin/koha/opac-detail.pl?biblionumber=1396"},{"id":367438,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Nepal","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"compilers":[{"text":"Evett, W. W.","contributorId":218997,"corporation":false,"usgs":false,"family":"Evett","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":770958,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"authors":[{"text":" Nepal Hydrological Survey Department.","contributorId":218998,"corporation":true,"usgs":false,"organization":" Nepal Hydrological Survey Department.","id":770957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70205377,"text":"70205377 - 1967 - Exploration for artesian water in the Sokoto Basin, Nigeria","interactions":[],"lastModifiedDate":"2024-03-22T00:11:13.530478","indexId":"70205377","displayToPublicDate":"1967-09-16T13:20:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Exploration for artesian water in the Sokoto Basin, Nigeria","docAbstract":"The Sokoto basin in semiarid northwestern Nigeria contains Cretaceous and Tertiary semiconsolidated deposits that dip gently northwest off an oldland of pre-Cretaceous crystalline rocks. Until recent years the dug well has been the chief source of ground water for the Hausa cultivators and the pastoral Fulani inhabitants of the region. Borehole exploration sponsored by US AID and the Geological Survey of Nigeria with technical guidance from the writers of the U. S. Geological Survey has revealed that the basal section of the Gwandu Formation contains a productive artesian sand aquifer throughout a 5,700 square mile area. Transmissibilities of the aquifer proved to be as high as 180,000 Imperial gallons a day per foot but generally decrease towards the west. The free flow areas total about 1,000 square miles with pressure heads in boreholes up to + 83 feet above land surface and individual flows as great as 12,000 gallons per hour. Beneath the Gwandu, pressure aquifers in the Rima Group and the Gundumi Formation also produce flowing water in the lowland (fadama) of the Sokoto River. In the southern part of the basin, however, only one aquifer is present in the Cretaceous sequence, because the Gundumi aquifer is absent and the Rima aquifer apparently grades into the upper permeable section of the Illo Group. The quality of the water from all the pressure aquifers is generally quite good, although the iron content is high in places and salinity increases in the very deep aquifers.
","language":"English","publisher":"National Groundwater Association","doi":"10.1111/j.1745-6584.1967.tb03670.x","usgsCitation":"Anderson, H., and Ogilbee, W., 1967, Exploration for artesian water in the Sokoto Basin, Nigeria: Groundwater, v. 5, no. 3, p. 42-46, https://doi.org/10.1111/j.1745-6584.1967.tb03670.x.","productDescription":"5 p.","startPage":"42","endPage":"46","costCenters":[],"links":[{"id":367442,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Nigeria","otherGeospatial":"Sokoto Province","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[8.50029,4.77198],[7.46211,4.41211],[7.0826,4.46469],[6.69807,4.24059],[5.89817,4.26245],[5.3628,4.88797],[5.03357,5.6118],[4.32561,6.27065],[3.57418,6.2583],[2.6917,6.25882],[2.74906,7.87073],[2.72379,8.50685],[2.91231,9.13761],[3.22035,9.44415],[3.70544,10.06321],[3.60007,10.33219],[3.79711,10.73475],[3.57222,11.32794],[3.61118,11.66017],[3.68063,12.5529],[3.96728,12.95611],[4.10795,13.53122],[4.36834,13.74748],[5.44306,13.86592],[6.44543,13.49277],[6.82044,13.11509],[7.33075,13.09804],[7.80467,13.34353],[9.01493,12.82666],[9.52493,12.8511],[10.11481,13.27725],[10.70103,13.24692],[10.98959,13.38732],[11.5278,13.32898],[12.30207,13.03719],[13.08399,13.59615],[13.3187,13.55636],[13.99535,12.46157],[14.18134,12.48366],[14.57718,12.08536],[14.46819,11.90475],[14.41538,11.57237],[13.57295,10.79857],[13.30868,10.16036],[13.1676,9.64063],[12.95547,9.41777],[12.75367,8.71776],[12.21887,8.30582],[12.06395,7.79981],[11.83931,7.39704],[11.74577,6.98138],[11.05879,6.64443],[10.49738,7.05536],[10.11828,7.03877],[9.52271,6.45348],[9.23316,6.44449],[8.75753,5.47967],[8.50029,4.77198]]]},\"properties\":{\"name\":\"Nigeria\"}}]}","volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Anderson, H. R.","contributorId":67487,"corporation":false,"usgs":true,"family":"Anderson","given":"H. R.","affiliations":[],"preferred":false,"id":770966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ogilbee, William","contributorId":106093,"corporation":false,"usgs":true,"family":"Ogilbee","given":"William","email":"","affiliations":[],"preferred":false,"id":770967,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70205361,"text":"70205361 - 1967 - Stratigraphic and tectonic framework of Libya","interactions":[],"lastModifiedDate":"2019-09-17T08:39:02","indexId":"70205361","displayToPublicDate":"1967-09-16T10:20:55","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":605,"text":"AAPG Bulletin","printIssn":"0149-1423","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphic and tectonic framework of Libya","docAbstract":"Libya is situated on the Mediterranean foreland of the African shield. Marine strata of Paleozoic, Mesozoic, and Cenozoic ages abound in northern Libya, but continental rocks of Paleozoic and Mesozoic ages predominate in southern Libya. Marine incursions in Ordovician, Silurian, Devonian, Carboniferous, late Cretaceous, and early Tertiary times reached far into the country, some crossing the southern border. Compressional folds are almost wholly absent, but uplift, subsidence, block faulting, and tilting have occurred, and angular and parallel unconformities are common. The major diastrophic disturbances include the Caledonian and Hercynian, as well as disturbances during late Cretaceous and Oligocene through Miocene or Recent times. The chief regional structures are the Gefara basin, Hamada basin, Gargaf arch, Marzuq basin, Tibesti-Haruj uplift, Kufra basin, Cyrenaican uplift, and Sirte embayment. Several large basalt flows of Cenozoic age are present. Sand and gravel conceal the bedrock in about a third of the country. In the Sirte embayment marine sedimentation, differential compaction, reef development, subsidence, and block faulting, beginning in late Cretaceous time, favored the development of source and reservoir rocks. Recoverable oil has been found chiefly in limestone and sandstone of early and late Cretaceous and Tertiary ages, and in knobs of probable early Paleozoic sandstone and in fractured granite. In the Hamada basin oil accumulations have been found in sandstones of Triassic age and of several Paleozoic systems. Most of the oil and gas discovered to date in Libya are in anticlinal structures, but several unconformities within the section probably influenced these accumulations; oil and gas may well await discovery in other types of traps.
","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/5D25C0C9-16C1-11D7-8645000102C1865D","issn":"0002-7464","usgsCitation":"Conant, L., and Goudarzi, G., 1967, Stratigraphic and tectonic framework of Libya: AAPG Bulletin, v. 51, no. 5, p. 719-730, https://doi.org/10.1306/5D25C0C9-16C1-11D7-8645000102C1865D.","productDescription":"12 p.","startPage":"719","endPage":"730","numberOfPages":"12","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":367425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Libya","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[14.8513,22.86295],[14.14387,22.49129],[13.58142,23.04051],[11.99951,23.47167],[11.56067,24.09791],[10.77136,24.56253],[10.30385,24.37931],[9.94826,24.93695],[9.91069,25.36545],[9.31941,26.09432],[9.71629,26.51221],[9.62906,27.14095],[9.75613,27.68826],[9.68388,28.14417],[9.86,28.95999],[9.80563,29.42464],[9.48214,30.30756],[9.97002,30.53932],[10.05658,30.96183],[9.95023,31.37607],[10.6369,31.76142],[10.94479,32.08181],[11.43225,32.3689],[11.48879,33.137],[12.66331,32.79278],[13.08326,32.87882],[13.91868,32.71196],[15.24563,32.26508],[15.71394,31.37626],[16.61162,31.18218],[18.02109,30.76357],[19.08641,30.26639],[19.57404,30.52582],[20.05335,30.98576],[19.82033,31.75179],[20.13397,32.2382],[20.85452,32.7068],[21.54298,32.8432],[22.89576,32.63858],[23.2368,32.19149],[23.60913,32.18726],[23.9275,32.01667],[24.92114,31.89936],[25.16482,31.56915],[24.80287,31.08929],[24.95762,30.6616],[24.70007,30.04419],[25,29.23865],[25,25.6825],[25,22],[25,20.00304],[23.85,20],[23.83766,19.58047],[19.84926,21.49509],[15.86085,23.40972],[14.8513,22.86295]]]},\"properties\":{\"name\":\"Libya\"}}]}","volume":"51","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Conant, L. C.","contributorId":90381,"corporation":false,"usgs":true,"family":"Conant","given":"L. C.","affiliations":[],"preferred":false,"id":770933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goudarzi, G.H.","contributorId":103276,"corporation":false,"usgs":true,"family":"Goudarzi","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":770934,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70214101,"text":"70214101 - 1967 - Compilation of hydrologic data Green Creek, Brazos River basin, Texas, 1967","interactions":[],"lastModifiedDate":"2024-09-13T13:26:07.152429","indexId":"70214101","displayToPublicDate":"1967-09-12T11:42:37","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Compilation of hydrologic data Green Creek, Brazos River basin, Texas, 1967","docAbstract":"The U.S. Soil Conservation Service is actively engaged in the installation of flood and soil erosion reducing measures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found a total of 3,438 floodwater-retarding structures to be physically and economically feasible in Texas. As of September 30, 1967, 1,196 of these structures had been built.
This watershed-development program will have varying but important effects on the natural surface- and ground-water resources of river basins, especially where a large number of the floodwater-retarding structures are built. Basic hydrologic data under natural and developed conditions are needed to appraise the effects of the structures on the yield and mode of occurrence of runoff.
Hydrologic investigations of these small watersheds, both developed and undeveloped, were begun by the Geological Survey in 1951 and are now being made in 11 areas (fig. 1). These studies are being made in cooperation with the Texas Water Development Board, the Soil Conservation Service, the San Antonio River Authority, the city of Dallas and the Tarrant County Water Control and Improvement District No. 1. The 11 study areas were chosen to sample watersheds having different rainfall, topography, geology, and soils. In four of the study areas (North, Little Elm, Mukewater, and Pin Oak Creeks), streamflow and rainfall records were collected prior to construction of the floodwater-retarding structures, thus affording the opportunity for analyses of the conditions \"before and after\" development. Structures have now been built in three of these study areas. A summary of the development of the floodwater-retarding structures in each study area as of September 30, 1967, is shown in table 1.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70214101","collaboration":"Prepared in cooperation with Texas Water Development Board and Soil Conservation Service","usgsCitation":"U.S. Geological Survey, 1967, Compilation of hydrologic data Green Creek, Brazos River basin, Texas, 1967: Open-File Report, iii, 34 p., https://doi.org/10.3133/70214101.","productDescription":"iii, 34 p.","costCenters":[],"links":[{"id":425045,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70214101/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425044,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70214101/report-thumb.jpg"}],"country":"United 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