{"pageNumber":"5689","pageRowStart":"142200","pageSize":"25","recordCount":165635,"records":[{"id":70009941,"text":"70009941 - 1972 - Oil development and conservation in Arctic America","interactions":[],"lastModifiedDate":"2020-12-23T21:10:37.726271","indexId":"70009941","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Oil development and conservation in Arctic America","docAbstract":"

As in his earlier article to which reference is made, the author stresses the need for more background information and a much greater research effort before problems of environmental protection from oil developments in northern Alaska can be effectively tackled. Meanwhile, there are indications that the earlier estimates of around ten thousand million barrels should be raised—perhaps to about five times as much. There has moreover been a great increate also in the known and probable gas reserves in northern Canada—particularly in the Arctic Archipelago. In spite of planned automation, people will be needed for development—including Eskimos and Indians, whose interests will be widely protected under the Alaska Native Claims Settlement Act of December 1971. The International Biological Programme ‘Tundra Biome’ projects have accumulated much new information, including the results to be expected from disturbing the tundra seriously, and means of preventing or repairing damage to it. There is much interest in Alaska and Canada in protection of the northern environment, and in the former the US National Environmental Policy Act is already leading to stricter control of some developments.

","language":"English","publisher":"Elsevier","doi":"10.1016/0006-3207(72)90054-7","issn":"00063207","usgsCitation":"Reed, J., 1972, Oil development and conservation in Arctic America: Biological Conservation, v. 4, no. 5, p. 369-371, https://doi.org/10.1016/0006-3207(72)90054-7.","productDescription":"3 p.","startPage":"369","endPage":"371","numberOfPages":"3","costCenters":[],"links":[{"id":219117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6cf3e4b0c8380cd74eb8","contributors":{"authors":[{"text":"Reed, J. C.","contributorId":75589,"corporation":false,"usgs":true,"family":"Reed","given":"J. C.","affiliations":[],"preferred":false,"id":357498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010210,"text":"70010210 - 1972 - Oceanic ridges and transform faults: Their intersection angles and resistance to plate motion","interactions":[],"lastModifiedDate":"2020-12-23T00:48:15.006936","indexId":"70010210","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Oceanic ridges and transform faults: Their intersection angles and resistance to plate motion","docAbstract":"

The persistent near-orthogonal pattern formed by oceanic ridges and transform faults defies explanation in terms of rigid plates because it probably depends on the energy associated with deformation. For passive spreading, it is likely that the ridges and transforms adjust to a configuration offering minimum resistance to plate separation. This leads to a simple geometric model which yields conditions for the occurrence of transform faults and an aid to interpretation of structural patterns in the sea floor. Under reasonable assumptions, it is much more difficult for diverging plates to spread a kilometer of ridge than to slip a kilometer of transform fault, and the patterns observed at spreading centers might extend to lithospheric depths. Under these conditions, the resisting force at spreading centers could play a significant role in the dynamics of plate-tectonic systems.

","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(72)90051-9","issn":"0012821X","usgsCitation":"Lachenbruch, A., and Thompson, G.A., 1972, Oceanic ridges and transform faults: Their intersection angles and resistance to plate motion: Earth and Planetary Science Letters, v. 15, no. 2, p. 116-122, https://doi.org/10.1016/0012-821X(72)90051-9.","productDescription":"7 p.","startPage":"116","endPage":"122","numberOfPages":"7","costCenters":[],"links":[{"id":219000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6c9be4b0c8380cd74cfd","contributors":{"authors":[{"text":"Lachenbruch, A.H.","contributorId":76737,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"A.H.","affiliations":[],"preferred":false,"id":358315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, G. A.","contributorId":90332,"corporation":false,"usgs":true,"family":"Thompson","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":358316,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010211,"text":"70010211 - 1972 - Site distribution of iron in staurolite","interactions":[],"lastModifiedDate":"2020-12-23T00:45:42.632756","indexId":"70010211","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Site distribution of iron in staurolite","docAbstract":"

The Mössbauer spectrum of staurolite does not necessarily indicate that ferrous iron is distributed over both the tetrahedral Fe site and one or more of the octahedral sites, as previously thought. Two doublets are present in the spectrum, but their quadrupole spliting and isomer shift are more consistent with both being due to tetrahedrally coordinated ferrous iron. Smith's X-ray work has shown that cations in the Fe site actually assume several slightly different positions, and iron in each of these positions may give rise to a different Mössbauer doublet.

","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(72)90031-3","issn":"0012821X","usgsCitation":"Dowty, E., 1972, Site distribution of iron in staurolite: Earth and Planetary Science Letters, v. 15, no. 1, p. 72-74, https://doi.org/10.1016/0012-821X(72)90031-3.","productDescription":"3 p.","startPage":"72","endPage":"74","numberOfPages":"3","costCenters":[],"links":[{"id":219056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b90f2e4b08c986b3196f5","contributors":{"authors":[{"text":"Dowty, Eric","contributorId":30334,"corporation":false,"usgs":true,"family":"Dowty","given":"Eric","email":"","affiliations":[],"preferred":false,"id":358317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009812,"text":"70009812 - 1972 - Imaging experiment: The Viking Lander","interactions":[],"lastModifiedDate":"2020-12-23T21:39:11.875147","indexId":"70009812","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Imaging experiment: The Viking Lander","docAbstract":"

The Viking Lander Imaging System will consist of two identical facsimile cameras. Each camera has a high-resolution mode with an instantaneous field of view of 0.04°, and survey and color modes with instantaneous fields of view of 0.12°. Cameras are positioned one meter apart to provide stereoscopic coverage of the near-field. The Imaging Experiment will provide important information about the morphology, composition, and origin of the Martian surface and atmospheric features. In addition, lander pictures will provide supporting information for other experiments in biology, organic chemistry, meteorology, and physical properties.

","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(72)90139-X","issn":"00191035","usgsCitation":"Mutch, T., Binder, A., Huck, F., Levinthal, E., Morris, E.C., Sagan, C., and Young, A., 1972, Imaging experiment: The Viking Lander: Icarus, v. 16, no. 1, p. 92-110, https://doi.org/10.1016/0019-1035(72)90139-X.","productDescription":"19 p.","startPage":"92","endPage":"110","numberOfPages":"19","costCenters":[],"links":[{"id":218911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3881e4b0c8380cd615bd","contributors":{"authors":[{"text":"Mutch, T.A.","contributorId":61884,"corporation":false,"usgs":true,"family":"Mutch","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":357205,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Binder, A.B.","contributorId":86855,"corporation":false,"usgs":true,"family":"Binder","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":357207,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huck, F.O.","contributorId":106256,"corporation":false,"usgs":true,"family":"Huck","given":"F.O.","email":"","affiliations":[],"preferred":false,"id":357208,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Levinthal, E.C.","contributorId":45823,"corporation":false,"usgs":true,"family":"Levinthal","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":357204,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Morris, E. C.","contributorId":84381,"corporation":false,"usgs":true,"family":"Morris","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":357206,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sagan, C.","contributorId":42336,"corporation":false,"usgs":true,"family":"Sagan","given":"C.","email":"","affiliations":[],"preferred":false,"id":357203,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Young, A.T.","contributorId":17757,"corporation":false,"usgs":true,"family":"Young","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":357202,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":5220085,"text":"5220085 - 1972 - A repellent for protecting corn seed from blackbirds and crows","interactions":[],"lastModifiedDate":"2025-02-21T17:35:25.856939","indexId":"5220085","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"A repellent for protecting corn seed from blackbirds and crows","docAbstract":"

Methiocarb [4-(methylthio)-3,-5-xylyl N-methylcarbamate] was tested as a seed treatment for repelling blackbirds and crows (Corvus sp.) from sprouting corn in South Carolina. The test was conducted on eight fields within a 0.25-square-mile area. Marked repellency occurred; sprout damage averaged 44 percent in the control fields and 0.3 percent in the fields treated with methiocarb.

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Jr.","contributorId":14538,"corporation":false,"usgs":true,"family":"Stickley","given":"A.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":331311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guarineo, J.L.","contributorId":90411,"corporation":false,"usgs":true,"family":"Guarineo","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":331312,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001528,"text":"1001528 - 1972 - The sandhill crane with emphasis on aspects related to North Dakota","interactions":[],"lastModifiedDate":"2020-05-11T15:23:47.069139","indexId":"1001528","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3111,"text":"Prairie Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"The sandhill crane with emphasis on aspects related to North Dakota","docAbstract":"

No abstract available.

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E.","contributorId":37275,"corporation":false,"usgs":true,"family":"Lennon","given":"R.","middleInitial":"E.","affiliations":[],"preferred":false,"id":313013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175672,"text":"70175672 - 1972 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971","interactions":[],"lastModifiedDate":"2016-08-17T16:02:33","indexId":"70175672","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"29","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971","docAbstract":"

No abstract available.

","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Puente, C., 1972, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971: Edwards Underground Water District Bulletin 29, 8 p.","productDescription":"8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326771,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad1e4b03bcb0104bbca","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":645992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":81428,"text":"81428 - 1972 - Destruction of the ecosystem in the Great Lakes and possibilities for its reconstruction","interactions":[],"lastModifiedDate":"2012-02-02T00:03:51","indexId":"81428","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Destruction of the ecosystem in the Great Lakes and possibilities for its reconstruction","docAbstract":"This paper is a review of the sequence of events within the Great Lakes and their drainage to provide a basis for interpreting probable cause-and-effect relations between events of settlement and changes in the ecosystem of the Great Lakes. Possibilities of restoration of the lakes are discussed. A plan to do so must include (1) improvement of land uses in the drainage basin, (2) elimination of sources of physical, chemical, and biological pollution entering the lakes, and (3) restoration of favorable and productive fish populations.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Progress in fishery and food science","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Univ of Washington Publications in Fisheries","usgsCitation":"Smith, S.H., 1972, Destruction of the ecosystem in the Great Lakes and possibilities for its reconstruction, chap. of Progress in fishery and food science, v. 5, p. 41-46.","productDescription":"p. 41-46","startPage":"41","endPage":"46","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":126955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667d6b","contributors":{"editors":[{"text":"Moore, Remedios W.","contributorId":113125,"corporation":false,"usgs":true,"family":"Moore","given":"Remedios","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":504077,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":295350,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185775,"text":"70185775 - 1972 - Some rates of geomorphological processes","interactions":[],"lastModifiedDate":"2017-03-29T09:06:35","indexId":"70185775","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5345,"text":"Geographia Polonica","active":true,"publicationSubtype":{"id":10}},"title":"Some rates of geomorphological processes","docAbstract":"

This brief report summarizes three sets of measurement data on certain processes.

The first concerns the rate of movement of soil on hillslopes, especially by mass movement or slow gravitational creep. The results are abstracted from an unpublished manuscript by the junior author who reports on the measurements which Leopold began 10 or more years ago and to which in more recent years Emmett has added new sites and has carried on the annual remeasurement. The results are those from \"mass-movement lines\", which consist of a series of pins or iron rods, 10 inches (25 cm) long driven vertically into the ground along a straight line-of-sight, secured at each end with stiff iron posts. The Survey consists of setting a theodolite over one of the end bench marks and orienting on the other. The distance of each individual pin from the line of sight is recorded. Resurveys are usually made annually.

","language":"English","publisher":"Institute of Geography and Spatial Organization Polish Academy of Sciences","usgsCitation":"Leopold, L.B., and Emmett, W.W., 1972, Some rates of geomorphological processes: Geographia Polonica, v. 23, p. 27-36.","productDescription":"10 p.","startPage":"27","endPage":"36","costCenters":[],"links":[{"id":338514,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338513,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.geographiapolonica.pl/article/item/8673.html"}],"volume":"23","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc823e4b02ff32c685766","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686711,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":686712,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70194897,"text":"70194897 - 1972 - Duck hepatitis virus Interactions with DDT and dieldrin in adult mallards ","interactions":[],"lastModifiedDate":"2018-02-23T13:37:49","indexId":"70194897","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Duck hepatitis virus Interactions with DDT and dieldrin in adult mallards ","docAbstract":"

There has been considerable speculation regarding possible imteractlons within biological systems between synthetic environmental pollutants and infectious disease agents (1-11). This type of interaction has been studied in our laboratory using the mallard, Anas platyrhynchos, as a test species (5,6). Since adult ducks are refractory to the overt manifestations of duck virus hepatitis (DVH) (12) and because duck hepatitis virus (DHV) has a predilection for the liver, the organ responsible for the metabolism of many chemicals, (13) an experiment was undertaken to determine if infection with DHV had any effect on the toxicity to adult mallards of p,p'-DDT or technical grade dieldrin.

","language":"English","publisher":"Springer","doi":"10.1007/BF01684399","usgsCitation":"Friend, M., and Trainer, D., 1972, Duck hepatitis virus Interactions with DDT and dieldrin in adult mallards : Bulletin of Environmental Contamination and Toxicology, v. 7, no. 4, p. 202-206, https://doi.org/10.1007/BF01684399.","productDescription":"5 p.","startPage":"202","endPage":"206","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":350728,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6c4cb3e4b06e28e9cabb54","contributors":{"authors":[{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":726019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trainer, D.O.","contributorId":98674,"corporation":false,"usgs":true,"family":"Trainer","given":"D.O.","email":"","affiliations":[],"preferred":false,"id":726020,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010282,"text":"70010282 - 1972 - Electron microprobe evaluation of terrestrial basalts for whole-rock K-Ar dating","interactions":[],"lastModifiedDate":"2020-12-23T00:26:40.435978","indexId":"70010282","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Electron microprobe evaluation of terrestrial basalts for whole-rock K-Ar dating","docAbstract":"

Four basalt samples for whole-rock K-Ar dating were analyzed with an electron microprobe to locate potassium concentrations. Highest concentrations of potassium were found in those mineral phases which were the last to crystallize. The two reliable samples had potassium concentrated in fine-grained interstitial feldspar and along grain boundaries of earlier formed plagioclase crystals. The two unreliable samples had potassium concentrated in the glassy matrix, demonstrating the ineffectiveness of basaltic glass as a retainer of radiogenic argon. In selecting basalt samples for whole-rock K-Ar dating, particular emphasis should be placed on determining the nature and condition of the fine-grained interstitial phases.

","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(72)90262-2","issn":"0012821X","usgsCitation":"Mankinen, E., and Dalrymple, G.B., 1972, Electron microprobe evaluation of terrestrial basalts for whole-rock K-Ar dating: Earth and Planetary Science Letters, v. 17, no. 1, p. 89-94, https://doi.org/10.1016/0012-821X(72)90262-2.","productDescription":"6 p.","startPage":"89","endPage":"94","numberOfPages":"6","costCenters":[],"links":[{"id":219062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a08a8e4b0c8380cd51bf3","contributors":{"authors":[{"text":"Mankinen, E. A. 0000-0001-7496-2681","orcid":"https://orcid.org/0000-0001-7496-2681","contributorId":31786,"corporation":false,"usgs":true,"family":"Mankinen","given":"E. A.","affiliations":[],"preferred":false,"id":358514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dalrymple, G. Brent","contributorId":55146,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":358515,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010306,"text":"70010306 - 1972 - The geologic setting of the Luna 16 landing site","interactions":[],"lastModifiedDate":"2020-12-23T00:13:08.321055","indexId":"70010306","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"The geologic setting of the Luna 16 landing site","docAbstract":"

The Luna 16 landing site is similar in its geologic setting to Apollos 11 and 12. All three sites are located on basaltic mare fill which occurs mostly within multi-ring basins formed by impact earlier in the moon's history. A regolith developed by impact bombardment is present at each of these sites. The regolith is composed mostly of locally derived volcanic material, but also contains exotic fine fragments that have been ballistically transported into the landing sites by large impact events which formed craters such as Langrenus and Copernicus. These exotic fragments probably consist mostly of earlier reworked multi-ring basin debris and, although not directly traceable to individual sources, they do represent a good statistical sample of the composition of most of the premare terrac regions.

","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(72)90099-4","issn":"0012821X","usgsCitation":"McCauley, J., and Scott, D.H., 1972, The geologic setting of the Luna 16 landing site: Earth and Planetary Science Letters, v. 13, no. 2, p. 225-232, https://doi.org/10.1016/0012-821X(72)90099-4.","productDescription":"8 p.","startPage":"225","endPage":"232","numberOfPages":"8","costCenters":[],"links":[{"id":219522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bac5be4b08c986b323448","contributors":{"authors":[{"text":"McCauley, J.F.","contributorId":26310,"corporation":false,"usgs":true,"family":"McCauley","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":358586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, D. H.","contributorId":73565,"corporation":false,"usgs":true,"family":"Scott","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":358587,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70009762,"text":"70009762 - 1972 - Microcoulometric measurement of water in minerals","interactions":[],"lastModifiedDate":"2020-12-23T21:46:03.156376","indexId":"70009762","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Microcoulometric measurement of water in minerals","docAbstract":"

A DuPont Moisture Analyzer is used in a microcoulometric method for determining water in minerals. Certain modifications, which include the heating of the sample outside the instrument, protect the system from acid gases and insure the conversion of all hydrogen to water vapor. Moisture analyzer data are compared to concurrent data obtained by a modified Penfield method. In general, there is a positive bias of from 0.1 to 0.2% in the moisture analyzer results and a similarity of bias in minerals of the same kind. Inhomogeneity, sample size, and moisture pick-up are invoked to explain deviations. The method is particularly applicable to small samples.


","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)81898-5","issn":"00032670","usgsCitation":"Cremer, M., Elsheimer, H., and Escher, E., 1972, Microcoulometric measurement of water in minerals: Analytica Chimica Acta, v. 60, no. 1, p. 183-192, https://doi.org/10.1016/S0003-2670(01)81898-5.","productDescription":"10 p.","startPage":"183","endPage":"192","numberOfPages":"10","costCenters":[],"links":[{"id":219268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5672e4b0c8380cd6d5d1","contributors":{"authors":[{"text":"Cremer, M.","contributorId":28865,"corporation":false,"usgs":true,"family":"Cremer","given":"M.","email":"","affiliations":[],"preferred":false,"id":357080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elsheimer, H.N.","contributorId":77523,"corporation":false,"usgs":true,"family":"Elsheimer","given":"H.N.","email":"","affiliations":[],"preferred":false,"id":357081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Escher, E.E.","contributorId":94160,"corporation":false,"usgs":true,"family":"Escher","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":357082,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70009924,"text":"70009924 - 1972 - Graphical methods for representing form and stability of aqueous metal ions","interactions":[],"lastModifiedDate":"2020-12-23T21:25:30.006272","indexId":"70009924","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Graphical methods for representing form and stability of aqueous metal ions","docAbstract":"

The equilibrium distributions of solute species of aluminum at 25°C and one atmosphere pressure are shown graphically in systems containing fluoride, as functions of the total dissolved aluminum and fluoride. The predominant form of complex and degree of complexing are also shown graphically as functions of pH and fluoride activity. The graphs are based on the simultaneous solution of the equations representing nine complexing equilibria and three stoichiometric summarizations, using a fixed value of ionic strength equal to 0.1. Solubility relationships for aluminum hydroxide and cryolite also are shown graphically, using the same coordinates and additional equilibria. By overlaying an appropriate species distribution graph with a solubility graph a relatively complete summary of chemical relationships in an aqueous aluminum system can be obtained. Although this type of model has important limitations, it can accommodate enough variables simultaneously to have practical value and similar procedures could be used for other elements and systems of interest in low-temperature aqueous geochemistry.

","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(72)90042-3","issn":"00092541","usgsCitation":"Hem, J., 1972, Graphical methods for representing form and stability of aqueous metal ions: Chemical Geology, v. 9, no. 1-4, p. 119-132, https://doi.org/10.1016/0009-2541(72)90042-3.","productDescription":"14 p.","startPage":"119","endPage":"132","numberOfPages":"14","costCenters":[],"links":[{"id":218836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a29d3e4b0c8380cd5ac8e","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":357467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010094,"text":"70010094 - 1972 - Differentiation and volcanism in the lunar highlands: Photogeologic evidence and Apollo 16 implications","interactions":[],"lastModifiedDate":"2020-12-23T20:47:47.740182","indexId":"70010094","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Differentiation and volcanism in the lunar highlands: Photogeologic evidence and Apollo 16 implications","docAbstract":"

Materials of possible volcanic origin in the lunar highlands include (1) highland plains materials, (2) materials forming closely spaced hills in which summit furrows and chains of craters are common and (3) materials forming closely spaced hills (some of which parallel the lunar grid) on which summit furrows and chain craters are rare. The highland plains materials probably are basaltic lavas with less Fe and Ti than the mare plains materials. The two hilly units appear to consist of materials that, if volcanic, were more viscous in the molten state than any of the lunar plains units; thus these materials may be significantly enriched in felsic components. Most of the highland materials of possible volcanic origin formed after the Imbrium multi-ring basin but before mare material completed flooding parts of the moon; they therefore postdate accretion of the moon and may represent several episodes of premare volcanism.

","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(72)90007-6","issn":"0012821X","usgsCitation":"Trask, N., and McCauley, J., 1972, Differentiation and volcanism in the lunar highlands: Photogeologic evidence and Apollo 16 implications: Earth and Planetary Science Letters, v. 14, no. 2, p. 201-206, https://doi.org/10.1016/0012-821X(72)90007-6.","productDescription":"6 p.","startPage":"201","endPage":"206","numberOfPages":"6","costCenters":[],"links":[{"id":219665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0107e4b0c8380cd4fa62","contributors":{"authors":[{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":357882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCauley, J.F.","contributorId":26310,"corporation":false,"usgs":true,"family":"McCauley","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":357881,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010297,"text":"70010297 - 1972 - Prospects for earthquake prediction and control","interactions":[],"lastModifiedDate":"2020-03-19T08:29:15","indexId":"70010297","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Prospects for earthquake prediction and control","docAbstract":"

The San Andreas fault is viewed, according to the concepts of seafloor spreading and plate tectonics, as a transform fault that separates the Pacific and North American plates and along which relative movements of 2 to 6 cm/year have been taking place. The resulting strain can be released by creep, by earthquakes of moderate size, or (as near San Francisco and Los Angeles) by great earthquakes. Microearthquakes, as mapped by a dense seismograph network in central California, generally coincide with zones of the San Andreas fault system that are creeping. Microearthquakes are few and scattered in zones where elastic energy is being stored. Changes in the rate of strain, as recorded by tiltmeter arrays, have been observed before several earthquakes of about magnitude 4. Changes in fluid pressure may control timing of seismic activity and make it possible to control natural earthquakes by controlling variations in fluid pressure in fault zones. An experiment in earthquake control is underway at the Rangely oil field in Colorado, where the rates of fluid injection and withdrawal in experimental wells are being controlled. 

","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(72)90080-7","issn":"00401951","usgsCitation":"Healy, J.H., Lee, W., Pakiser, L.C., Raleigh, C., and Wood, M., 1972, Prospects for earthquake prediction and control: Tectonophysics, v. 14, no. 3-4, p. 319-332, https://doi.org/10.1016/0040-1951(72)90080-7.","productDescription":"14 p.","startPage":"319","endPage":"332","numberOfPages":"14","costCenters":[],"links":[{"id":219297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Andreas Fault","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.29980468749999,\n 35.06597313798418\n ],\n [\n -117.24609374999999,\n 35.06597313798418\n ],\n [\n -117.24609374999999,\n 42.13082130188811\n ],\n [\n -122.29980468749999,\n 42.13082130188811\n ],\n [\n -122.29980468749999,\n 35.06597313798418\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"14","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8f57e4b0c8380cd7f6e6","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":358553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, W.H.K.","contributorId":35303,"corporation":false,"usgs":true,"family":"Lee","given":"W.H.K.","affiliations":[],"preferred":false,"id":358551,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pakiser, L. C.","contributorId":83512,"corporation":false,"usgs":true,"family":"Pakiser","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358555,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Raleigh, C.B.","contributorId":40219,"corporation":false,"usgs":true,"family":"Raleigh","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":358552,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wood, M.D.","contributorId":63930,"corporation":false,"usgs":true,"family":"Wood","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":358554,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70010296,"text":"70010296 - 1972 - Biscalitheca suzanneana, N. Sp., from the uppermost Pennsylvanian of Texas","interactions":[],"lastModifiedDate":"2020-12-23T00:19:02.603377","indexId":"70010296","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3275,"text":"Review of Palaeobotany and Palynology","active":true,"publicationSubtype":{"id":10}},"title":"Biscalitheca suzanneana, N. Sp., from the uppermost Pennsylvanian of Texas","docAbstract":"

Biscalitheca suzanneana, n. sp., is described from specimens found in an uppermost Pennsylvanian deposit in north-central Texas. The genus was identified primarily on the basis of impressions of the unique sporangial annuli. The occurrence establishes for Biscalitheca a stratigraphic range equivalent to nearly the entire Upper Pennsylvanian Series.

","language":"English","publisher":"Elsevier","doi":"10.1016/0034-6667(72)90015-2","issn":"00346667","usgsCitation":"Mamay, S., 1972, Biscalitheca suzanneana, N. 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\"}}]}","volume":"14","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f1d0e4b0c8380cd4ae36","contributors":{"authors":[{"text":"Mamay, S.H.","contributorId":49422,"corporation":false,"usgs":true,"family":"Mamay","given":"S.H.","affiliations":[],"preferred":false,"id":358550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009763,"text":"70009763 - 1972 - A probe for neutron activation analysis in a drill hole using 252Cf, and a Ge(Li) detector cooled by a melting cryogen","interactions":[],"lastModifiedDate":"2020-12-23T21:43:28.539187","indexId":"70009763","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2906,"text":"Nuclear Instruments and Methods","active":true,"publicationSubtype":{"id":10}},"title":"A probe for neutron activation analysis in a drill hole using 252Cf, and a Ge(Li) detector cooled by a melting cryogen","docAbstract":"

A sonde has been built for high-resolution measurement of natural or neutron-induced gamma rays in boreholes. The sonde is 7.3 cm in diameter and about 2.2 m in length and weighs about 16 kg. The lithium-compensated germanium semiconductor detector is stabilized at −185 to −188°C for as much as ten hours by a cryostatic reservoir containing melting propane. During periods when the sonde is not in use the propane is kept frozen by a gravity-fed trickle of liquid nitrogen from a reservoir temporarily attached to the cryostat section. A 252Cf source, shielded from the detector, may be placed in the bottom section of the sonde for anlysis by measurement of neutron-activation or neutron-capture gamma rays. Stability of the cryostat with changing hydrostatic pressure, absence of vibration, lack of need for power to the cryostat during operation, and freedom of orientation make the method desirable for borehole, undersea, space, and some laboratory applications.

","language":"English","publisher":"Elsevier","doi":"10.1016/0029-554X(72)90262-5","issn":"0029554X","usgsCitation":"Tanner, A., Moxham, R., Senftle, F.E., and Baicker, J., 1972, A probe for neutron activation analysis in a drill hole using 252Cf, and a Ge(Li) detector cooled by a melting cryogen: Nuclear Instruments and Methods, v. 100, no. 1, p. 1-7, https://doi.org/10.1016/0029-554X(72)90262-5.","productDescription":"7 p.","startPage":"1","endPage":"7","numberOfPages":"7","costCenters":[],"links":[{"id":219328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"100","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e509e4b0c8380cd46aa8","contributors":{"authors":[{"text":"Tanner, A.B.","contributorId":44155,"corporation":false,"usgs":true,"family":"Tanner","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":357085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":357084,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357086,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baicker, J.A.","contributorId":8870,"corporation":false,"usgs":true,"family":"Baicker","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":357083,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1014327,"text":"1014327 - 1972 - Studies on the control of whirling disease (Myxosoma cerebralis)","interactions":[],"lastModifiedDate":"2025-04-07T15:23:32.021842","indexId":"1014327","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Studies on the control of whirling disease (Myxosoma cerebralis)","docAbstract":"

Based on presumptive evidence of death (extrusion of polar filaments and disintegration of sporoplasm) 1.0%, 0.5%, and 0.25% calcium oxide or potassium hydroxide killed the spores of Myxosoma cerebrallis in vitro. Chlorine at 400 ppm destroyed 36% to 90% of the spores but 13% to 37% of those in the controls perished. Calcium hydroxide, ammonium chloride, sodium borate, potassium permanganate, Roccal (alkyl dimethylbenzylammonium chloride), and copper sulfate allowed survival of 38–96% of the spores, usually not much less than the rate of survival of the controls.

In simulated pond testing, quicklime at 380 grams or more per square meter (3360 lbs/acre) of pond bottom prevented whirling disease in rainbow trout (Salmo gairdneri).

","language":"English","publisher":"BioOne","doi":"10.7589/0090-3558-8.1.49","usgsCitation":"Hoffman, G., and Hoffman, G., 1972, Studies on the control of whirling disease (Myxosoma cerebralis): Journal of Wildlife Diseases, v. 8, no. 1, p. 49-53, https://doi.org/10.7589/0090-3558-8.1.49.","productDescription":"5 p.","startPage":"49","endPage":"53","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":488601,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-8.1.49","text":"Publisher Index Page"},{"id":131067,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d48","contributors":{"authors":[{"text":"Hoffman, G.L. Sr.","contributorId":62963,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.L.","suffix":"Sr.","email":"","affiliations":[],"preferred":false,"id":320203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, G.L. Jr.","contributorId":102030,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.L.","suffix":"Jr.","affiliations":[],"preferred":false,"id":320204,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010142,"text":"70010142 - 1972 - Occurrence of chromian, hercynitic spinel (\"pleonaste\") in Apollo-14 samples and its petrologic implications","interactions":[],"lastModifiedDate":"2020-12-23T01:13:11.010862","indexId":"70010142","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of chromian, hercynitic spinel (\"pleonaste\") in Apollo-14 samples and its petrologic implications","docAbstract":"

Many isolated grains of a reddish pleonaste-type spinel occur in fines and metabreccia samples, particularly 14 319. Electron microprobe analyses (104) of spinels and their associated phases include 58 of pleonaste which show Mg/(Mg + Fe) 0.44–0.62 and Cr/(Cr + Al) 0.017–0.134 (atomic), plus minor amounts of other ions, and differ greatly from almost all previously recorded lunar spinels; almost no spinels of intermediate composition were found. Two types of compositional zoning exist: a diffuse primary one with cores lower in Ti, and a narrow secondary one from reaction with matrix yielding rims higher in Cr, Ti, and Mn. At contacts with breccia matrix there is a narrow corona of almost pure plagioclase (An80-An94), free of opaque minerals and pyroxene. Two types of solid inclusions found in the pleonaste are calcic plagioclase, and tiny spherical masses of nickel-rich sulfide.

Similar pleonaste occurs in crystalline rock clasts, mainly with plagioclase; one clast (A) consists only of coarse olivine, plagioclase, and pleonaste, with granulated grain boundaries suggestive of deformation. From composition and texture, this clast is one possible candidate for the mafic cumulate counterpart of the “anorthositic” crust. Another clast (B), also made solely of olivine, plagioclase and pleonaste, is itself a breccia. These data suggest a two-stage brecciation process: 1) disruption (probably pre-Imbrian) of a deep-seated pleonaste-bearing source rock like A and reconsolidation to form a breccia without addition of pyroxene, ilmenite or other minerals; and 2) disruption of this breccia to yield breccia clast B which was then incorporated into the Fra Mauro formation.

","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(72)90038-6","issn":"0012821X","usgsCitation":"Roedder, E., and Weiblen, P., 1972, Occurrence of chromian, hercynitic spinel (\"pleonaste\") in Apollo-14 samples and its petrologic implications: Earth and Planetary Science Letters, v. 15, no. 4, p. 376-402, https://doi.org/10.1016/0012-821X(72)90038-6.","productDescription":"27 p.","startPage":"376","endPage":"402","numberOfPages":"27","costCenters":[],"links":[{"id":219216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6bd8e4b0c8380cd7490b","contributors":{"authors":[{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":358100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiblen, P.W.","contributorId":31884,"corporation":false,"usgs":true,"family":"Weiblen","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":358099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000385,"text":"1000385 - 1972 - Factors of ecologic succession in oligotrophic fish communities of the Laurentian Great Lakes","interactions":[],"lastModifiedDate":"2016-03-14T13:12:54","indexId":"1000385","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Factors of ecologic succession in oligotrophic fish communities of the Laurentian Great Lakes","docAbstract":"

Oligotrophic fish communities of the Great Lakes have undergone successive disruptions since the mid-1800s. Major contributing factors have been intensive selective fisheries, extreme modification of the drainage, invasion of marine species, and progressive physical–chemical changes of the lake environments. Lake Ontario was the first to be affected as its basin was settled and industrialized earliest, and it was the first to be connected by canals to the mid-Atlantic where the alewife (Alosa pseudoharengus) and sea lamprey (Petromyzon marinus) which ultimately became established in the Great Lakes were abundant. Oligotrophic fish communities were successively disrupted in Lakes Erie, Huron, Michigan, and Superior as the affects of population growth, industrialization, and marine invaders spread upward in the Laurentian drainage.The degree and sequence of response of families offish and species within families differed for each factor, but the sequence of change among families and species has been the same in response to each factor as it affected various lakes at different times. The ultimate result of the disruption of fish communities has been a reduction of productivity of oligotrophic species that ranges from extreme in Lake Ontario to moderate in Lake Superior, and which has reached a state of instability and rapid change in the upper three Great Lakes by the rnid-1900s similar to the situation in Lake Ontario in the mid-1800s. Since oligotrophic species (primarily salmonines, coregonines, and deepwater cottids) are the only kinds of fish that fully occupied the entire volume of the deepwater Great Lakes (Ontario, Huron, Michigan, and Superior), the fish biomass of these lakes has been reduced as various species declined or disappeared. In Lake Erie, which is shallow, and in the shallow bays of the deep lakes, oligotrophic species were replaced by mesotrophic species, primarily percids, which have successively increased and declined. All oligotrophic species are greatly reduced or extinct in lakes Ontario and Erie, and are in various stages of decline in lakes Huron, Michigan, and Superior, from greatest to least, respectively. The percids appear to be near the end of their sequence of succession in lakes Erie, Ontario, and Huron (primarily Saginaw Bay) where only the yellow perch (Perca flavescens) remains abundant. The yellow perch appears to be on the brink of decline in Lake Erie, which has been more severely influenced by water quality change than the other lakes.

","language":"English","publisher":"NRC Research Press","doi":"10.1139/f72-117","usgsCitation":"Smith, S.H., 1972, Factors of ecologic succession in oligotrophic fish communities of the Laurentian Great Lakes: Journal of the Fisheries Research Board of Canada, v. 29, no. 6, p. 717-730, https://doi.org/10.1139/f72-117.","productDescription":"14 p.","startPage":"717","endPage":"730","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7a50","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308489,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5719,"text":"pp655G - 1972 - Channel changes of the Gila River in Safford Valley, Arizona, 1846-1970","interactions":[],"lastModifiedDate":"2024-11-18T18:57:19.921701","indexId":"pp655G","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"655","chapter":"G","title":"Channel changes of the Gila River in Safford Valley, Arizona, 1846-1970","docAbstract":"

No abstract available.

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A day and a half were spent on September 15 and 16, 1943 in a reconnaissance study of the old glass sand quarries in the Cheshire Quartzite near Cheshire, Massachusetts.

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