Recent Monte Carlo studies have documented the value of generalized least squares (GLS) procedures to estimate empirical relationships between streamflow statistics and physiographic basin characteristics. This paper presents a number of extensions of the GLS method that deal with realities and complexities of regional hydrologic data sets that were not addressed in the simulation studies. These extensions include: (1) a more realistic model of the underlying model errors; (2) smoothed estimates of cross correlation of flows; (3) procedures for including historical flow data; (4) diagnostic statistics describing leverage and influence for GLS regression; and (5) the formulation of a mathematical program for evaluating future gaging activities.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(89)90268-0","issn":"00221694","usgsCitation":"Tasker, G.D., and Stedinger, J., 1989, An operational GLS model for hydrologic regression: Journal of Hydrology, v. 111, no. 1-4, p. 361-375, https://doi.org/10.1016/0022-1694(89)90268-0.","productDescription":"15 p.","startPage":"361","endPage":"375","costCenters":[],"links":[{"id":224293,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eaa3e4b0c8380cd489ad","contributors":{"authors":[{"text":"Tasker, Gary D.","contributorId":83097,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":370277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stedinger, J.R.","contributorId":90733,"corporation":false,"usgs":true,"family":"Stedinger","given":"J.R.","affiliations":[],"preferred":false,"id":370278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70015594,"text":"70015594 - 1989 - Subduction of the Daiichi Kashima Seamount in the Japan trench","interactions":[],"lastModifiedDate":"2025-08-20T16:04:38.161889","indexId":"70015594","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Subduction of the Daiichi Kashima Seamount in the Japan trench","docAbstract":"In 1984-1985, the Kaiko consortium collected Seabeam, single-channel seismic and submersible sampling data in the vicinity of the Daiichi-Kashima seamount and the southern Japan trench. We performed a prestack migration of a Shell multichannel seismic profile, that crosses this area, and examined it in the light of this unusually diverse Kaiko dataset. Unlike the frontal structure of the northern Japan trench, where mass-wasting appears to be the dominant tectonic process, the margin in front of the Daiichi-Kashima shows indentation, imbrication, uplift and erosion. Emplacement of the front one-third of the seamount beneath the margin front occurs without accretion. We conclude that the Daiichi-Kashima seamount exemplifies an intermediate stage between the initial collision and subduction of a seamount at a continental margin.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(89)90393-4","issn":"00401951","usgsCitation":"Lallemand, S., Culotta, R., and von Huene, R.E., 1989, Subduction of the Daiichi Kashima Seamount in the Japan trench: Tectonophysics, v. 160, no. 1-4, p. 237-247, https://doi.org/10.1016/0040-1951(89)90393-4.","productDescription":"11 p.","startPage":"237","endPage":"247","costCenters":[],"links":[{"id":224105,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","otherGeospatial":"Daiichi Kashima","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 138.85496532918535,\n 36.519758676508644\n ],\n [\n 138.85496532918535,\n 35.26197948632307\n ],\n [\n 141.09421405790607,\n 35.26197948632307\n ],\n [\n 141.09421405790607,\n 36.519758676508644\n ],\n [\n 138.85496532918535,\n 36.519758676508644\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"160","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d0fe4b08c986b31d60b","contributors":{"authors":[{"text":"Lallemand, S.","contributorId":99703,"corporation":false,"usgs":true,"family":"Lallemand","given":"S.","email":"","affiliations":[],"preferred":false,"id":371323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Culotta, Ray","contributorId":97254,"corporation":false,"usgs":true,"family":"Culotta","given":"Ray","affiliations":[],"preferred":false,"id":371322,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"von Huene, Roland E. 0000-0003-1301-3866 rvonhuene@usgs.gov","orcid":"https://orcid.org/0000-0003-1301-3866","contributorId":191070,"corporation":false,"usgs":true,"family":"von Huene","given":"Roland","email":"rvonhuene@usgs.gov","middleInitial":"E.","affiliations":[{"id":7065,"text":"USGS emeritus","active":true,"usgs":false},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":371321,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70016145,"text":"70016145 - 1989 - Diffusion and consumption of methane in an unsaturated zone in north-central Illinois, U.S.A.","interactions":[],"lastModifiedDate":"2025-04-24T17:02:59.482645","indexId":"70016145","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Diffusion and consumption of methane in an unsaturated zone in north-central Illinois, U.S.A.","docAbstract":"The distribution of CH4 in unsaturated glacial and eolian deposits adjacent to buried low-level radioactive waste was measured, and movement of the gas from the waste source was simulated using a two-dimensional finite-difference model for gas diffusion in the unsaturated zone. Mean PCH4 was greatest (1.56 Pa) in a pebbly-sand deposit 11.6 m below the land surface and 12 m from the waste, and generally decreased with increased horizontal distance from the waste. Mean PCH4 was least (0.07 Pa) at depth of 1.8 m below land surface, regardless of distance from the waste. PCH4 at the land surface averaged 0.17 Pa. Depth versus PCH4 profiles suggest consumption of both waste-produced and atmospheric CH4 in the upper unsaturated zone, presumably by methanotrophic microorganisms. Numerical simulations of methane movement support the consumption observation; inclusion of a term in the model for consumption of CH4 in the upper 2 m of the unsaturated zone resulted in simulated PCH4 within 30% of mean PCH4 at eleven of thirteen sampling locations. A similar fit of the data was obtained for only four locations when consumption was not considered.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(89)90256-4","issn":"00221694","usgsCitation":"Striegl, R.G., and Ishii, A.L., 1989, Diffusion and consumption of methane in an unsaturated zone in north-central Illinois, U.S.A.: Journal of Hydrology, v. 111, no. 1-4, p. 133-143, https://doi.org/10.1016/0022-1694(89)90256-4.","productDescription":"11 p.","startPage":"133","endPage":"143","costCenters":[],"links":[{"id":222836,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois","county":"Bureau County","city":"Sheffield","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.6309,41.5867],[-89.6266,41.5862],[-89.5179,41.5867],[-89.5124,41.5867],[-89.4025,41.5862],[-89.3945,41.5862],[-89.338,41.5866],[-89.335,41.5866],[-89.3337,41.5866],[-89.2859,41.5856],[-89.2766,41.5856],[-89.168,41.5845],[-89.1676,41.5418],[-89.1672,41.4964],[-89.1668,41.4542],[-89.1664,41.4079],[-89.1654,41.3661],[-89.1649,41.3221],[-89.165,41.3099],[-89.1803,41.309],[-89.1962,41.3113],[-89.2078,41.3127],[-89.2249,41.3137],[-89.25,41.3205],[-89.2646,41.3219],[-89.2677,41.3219],[-89.2732,41.3206],[-89.275,41.3192],[-89.2824,41.3138],[-89.3124,41.3047],[-89.3344,41.3007],[-89.3387,41.298],[-89.3405,41.2957],[-89.3405,41.2934],[-89.3406,41.2889],[-89.3387,41.2853],[-89.3375,41.2816],[-89.3381,41.2775],[-89.3449,41.263],[-89.3479,41.2567],[-89.351,41.249],[-89.3553,41.2336],[-89.3926,41.2336],[-89.4665,41.2336],[-89.4659,41.1488],[-89.6392,41.1487],[-89.6394,41.2331],[-89.7414,41.2339],[-89.7554,41.2338],[-89.8568,41.2345],[-89.8572,41.3207],[-89.8559,41.4088],[-89.8555,41.4523],[-89.8563,41.4973],[-89.8564,41.5191],[-89.8601,41.519],[-89.861,41.5858],[-89.7481,41.586],[-89.7444,41.586],[-89.6309,41.5867]]]},\"properties\":{\"name\":\"Bureau\",\"state\":\"IL\"}}]}","volume":"111","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a010fe4b0c8380cd4faa0","contributors":{"authors":[{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true}],"preferred":false,"id":372658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ishii, A. L.","contributorId":61464,"corporation":false,"usgs":true,"family":"Ishii","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":372657,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70015741,"text":"70015741 - 1989 - Spark ablation-inductively coupled plasma spectrometry for analysis of geologic materials","interactions":[],"lastModifiedDate":"2025-08-14T15:51:38.704236","indexId":"70015741","displayToPublicDate":"2001-10-25T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3517,"text":"Talanta","active":true,"publicationSubtype":{"id":10}},"title":"Spark ablation-inductively coupled plasma spectrometry for analysis of geologic materials","docAbstract":"Spark ablation—inductively coupled plasma (SA-ICP) spectrometry is applied to the measurement of hafnium—zirconium ratios in zircons and to the determination of cerium, cobalt, iron, lead, nickel and phosphorus in ferromanganese nodules. Six operating parameters used for the high-voltage spark and argon-ICP combination are established by sequential simplex optimization of both signal-to-background ratio and signal-to-noise ratio. The time-dependences of the atomic emission signals of analytes and matrix elements ablated from a finely pulverized sample embedded in a pressed disk of copper demonstrate selective sampling by the spark. Concentration ratios of hafnium to zirconium in zircons are measured with a precision of 4% (relative standard deviation, RSD). For ferromanganese nodules, spectral measurements based on intensity ratios of analyte line to the Mn(II) 257.610 nm line provide precisions of analysis in the range from 7 to 14% RSD. The accuracy of analysis depends on use of standard additions of the reference material USGS Nod P-1, and an independent measurement of the Mn concentration.
","language":"English","publisher":"Elsevier","doi":"10.1016/0039-9140(89)80110-9","issn":"00399140","usgsCitation":"Golightly, D.W., Montaser, A., Smith, B., and Dorrzapf, A.F., 1989, Spark ablation-inductively coupled plasma spectrometry for analysis of geologic materials: Talanta, v. 36, no. 1-2, p. 299-303, https://doi.org/10.1016/0039-9140(89)80110-9.","productDescription":"5 p.","startPage":"299","endPage":"303","costCenters":[],"links":[{"id":223953,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b940fe4b08c986b31a83e","contributors":{"authors":[{"text":"Golightly, D. W.","contributorId":32922,"corporation":false,"usgs":true,"family":"Golightly","given":"D.","middleInitial":"W.","affiliations":[],"preferred":false,"id":371661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Montaser, A.","contributorId":19297,"corporation":false,"usgs":true,"family":"Montaser","given":"A.","email":"","affiliations":[],"preferred":false,"id":371660,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, B.L.","contributorId":39740,"corporation":false,"usgs":true,"family":"Smith","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":371662,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dorrzapf, A. F. Jr.","contributorId":65998,"corporation":false,"usgs":true,"family":"Dorrzapf","given":"A.","suffix":"Jr.","middleInitial":"F.","affiliations":[],"preferred":false,"id":371663,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70016010,"text":"70016010 - 1989 - The influence of reagent type on the kinetics of ultrafine coal flotation","interactions":[],"lastModifiedDate":"2025-06-24T16:58:39.32737","indexId":"70016010","displayToPublicDate":"2001-10-05T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3107,"text":"Powder Technology","active":true,"publicationSubtype":{"id":10}},"title":"The influence of reagent type on the kinetics of ultrafine coal flotation","docAbstract":"A kinetic study has been conducted to determine the influence of reagent type on flotation rates of ultrafine coal. Two ultrafine coal samples, the Illinois No. 5 (Springfield) and Pittsburgh No. 8, have been evaluated with various reagent types in order to derive the rate constants for coal (kc), ash (ka), and pyrite (kc). The reagents used in the study include anionic surfactants, anionic surfactant—alcohol mixtures, and frothing alcohols.
In general, the surfactant-alcohol mixtures tend to float ultrafine coal at a rate three to four times faster than either pure alcohols or pure anionic surfactants. Pine oil, a mixture of terpene alcohols and hydrocarbons, was an exception to this finding; it exhibited higher rate constants than the pure aliphatic alcohols or other pure anionic surfactants studied; this may be explained by the fact that the sample of pine oil used (70% alpha-terpineol) acted as a frother/collector system similar to alcohol/kerosene. The separation efficiencies of ash and pyrite from coal, as evidenced by the ratios of kc/ka or kc/kp, tend to indicate, however, that commercially available surfactant—alcohol mixtures are not as selective as pure alcohols such as 2-ethyl-1-hexanol or methylisobutylcarbinol.
Some distinct differences in various rate constants, or their ratios, were noted between the two coals studied, and are possibly attributable to surface chemistry effects.
","language":"English","publisher":"Elsevier","doi":"10.1016/0032-5910(89)80061-0","issn":"00325910","usgsCitation":"Read, R., Camp, L., Summers, M., and Rapp, D., 1989, The influence of reagent type on the kinetics of ultrafine coal flotation: Powder Technology, v. 59, no. 3, p. 153-162, https://doi.org/10.1016/0032-5910(89)80061-0.","productDescription":"10 p.","startPage":"153","endPage":"162","costCenters":[],"links":[{"id":223295,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bad35e4b08c986b323a60","contributors":{"authors":[{"text":"Read, R.B.","contributorId":31119,"corporation":false,"usgs":true,"family":"Read","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":372334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Camp, L.R.","contributorId":108235,"corporation":false,"usgs":true,"family":"Camp","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":372337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Summers, M.S.","contributorId":47087,"corporation":false,"usgs":true,"family":"Summers","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":372335,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rapp, D.M.","contributorId":105439,"corporation":false,"usgs":true,"family":"Rapp","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":372336,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":26521,"text":"wri894056 - 1989 - Low-flow profiles of the upper Chattahoochee River and tributaries in Georgia","interactions":[],"lastModifiedDate":"2017-01-25T10:03:26","indexId":"wri894056","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4056","title":"Low-flow profiles of the upper Chattahoochee River and tributaries in Georgia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri894056","usgsCitation":"Carter, R., Hopkins, E.H., and Perlman, H., 1989, Low-flow profiles of the upper Chattahoochee River and tributaries in Georgia: U.S. Geological Survey Water-Resources Investigations Report 89-4056, iv, 194 p. :ill. ;28 cm., https://doi.org/10.3133/wri894056.","productDescription":"iv, 194 p. :ill. ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":55386,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4056/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4056/report-thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"Upper Chattahoochee River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.166259765625,\n 34.45221847282654\n ],\n [\n -84.17724609375,\n 35.003003395276714\n ],\n [\n -83.38623046874997,\n 34.99400375757575\n ],\n [\n -83.38623046874997,\n 34.45221847282654\n ],\n [\n -84.166259765625,\n 34.45221847282654\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6487af","contributors":{"authors":[{"text":"Carter, R.F.","contributorId":101261,"corporation":false,"usgs":true,"family":"Carter","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":196541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hopkins, E. H.","contributorId":18411,"corporation":false,"usgs":true,"family":"Hopkins","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":196539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perlman, H.A.","contributorId":84406,"corporation":false,"usgs":true,"family":"Perlman","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":196540,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70015289,"text":"70015289 - 1989 - Chemical affinities between the solvent extractable and the bulk organic matter of fossil resin associated with an extinct podocarpaceae","interactions":[],"lastModifiedDate":"2025-06-23T17:01:28.582943","indexId":"70015289","displayToPublicDate":"2001-03-15T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3078,"text":"Phytochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Chemical affinities between the solvent extractable and the bulk organic matter of fossil resin associated with an extinct podocarpaceae","docAbstract":"Analyses by GC-MS and GC-IR of resin associated to Dacridiumites mawsonii deposits, an extinct species of Podocarpaceae occurring on the South Island of New Zealand during the Bortonian (Middle Eocene), have revealed that dehydroabietic acid is the predominant component of the solvent soluble fraction. Accordingly, this diterpenoid has been selected as the principal component material for spectroscopic comparison with the bulk resin using IR and CP/MAS 13C NMR.
","language":"English","publisher":"Elsevier","doi":"10.1016/0031-9422(89)80202-X","issn":"00319422","usgsCitation":"Grimalt, J., Simoneit, B.R., and Hatcher, P.G., 1989, Chemical affinities between the solvent extractable and the bulk organic matter of fossil resin associated with an extinct podocarpaceae: Phytochemistry, v. 28, no. 4, p. 1167-1171, https://doi.org/10.1016/0031-9422(89)80202-X.","productDescription":"5 p.","startPage":"1167","endPage":"1171","costCenters":[],"links":[{"id":224143,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"New Zealand","otherGeospatial":"South Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 171.56181164146744,\n -40.18324843710634\n ],\n [\n 167.80251720151884,\n -43.748579175990706\n ],\n [\n 164.92683934377834,\n -46.95158994515671\n ],\n [\n 171.1012964563227,\n -47.383588239975715\n ],\n [\n 173.89423129470677,\n -43.96416144271794\n ],\n [\n 174.74382191034056,\n -40.839488971906995\n ],\n [\n 171.56181164146744,\n -40.18324843710634\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"28","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f515e4b0c8380cd4c089","contributors":{"authors":[{"text":"Grimalt, J.O.","contributorId":51920,"corporation":false,"usgs":true,"family":"Grimalt","given":"J.O.","email":"","affiliations":[],"preferred":false,"id":370554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simoneit, Bernd R. T.","contributorId":51021,"corporation":false,"usgs":true,"family":"Simoneit","given":"Bernd","email":"","middleInitial":"R. T.","affiliations":[],"preferred":false,"id":370553,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hatcher, Patrick G.","contributorId":93625,"corporation":false,"usgs":true,"family":"Hatcher","given":"Patrick","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":370555,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70016015,"text":"70016015 - 1989 - 1,3,5-Hydroxybenzene structures in mosses","interactions":[],"lastModifiedDate":"2025-06-23T16:50:22.858427","indexId":"70016015","displayToPublicDate":"2001-03-15T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3078,"text":"Phytochemistry","active":true,"publicationSubtype":{"id":10}},"title":"1,3,5-Hydroxybenzene structures in mosses","docAbstract":"A number of mosses from widely different families have been studied by cross polarization solid state 13C NMR spectroscopy. Although polysaccharide-type materials dominate the NMR spectra, significant amounts of aromatic carbons are observed in some mosses. Some of this material can be removed by ultrasonic bath treatment, and is lignin derived, probably from impurities from fine root material from associated higher plants. However other material is truly moss-derived and appears to be from 1,3,5-hydroxybenzene structures. This is inconsistent with lignin as being a component of mosses, and suggests a tannin or hydroxybenzofuran polymer is responsible for moss rigidity.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0031-9422(00)97754-9","issn":"00319422","usgsCitation":"Wilson, M.A., Sawyer, J., Hatcher, P.G., and Lerch, H.E., 1989, 1,3,5-Hydroxybenzene structures in mosses: Phytochemistry, v. 28, no. 5, p. 1395-1400, https://doi.org/10.1016/S0031-9422(00)97754-9.","productDescription":"6 p.","startPage":"1395","endPage":"1400","costCenters":[],"links":[{"id":223396,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e21fe4b0c8380cd4598c","contributors":{"authors":[{"text":"Wilson, M. A.","contributorId":107649,"corporation":false,"usgs":false,"family":"Wilson","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":372349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sawyer, J.","contributorId":28015,"corporation":false,"usgs":true,"family":"Sawyer","given":"J.","affiliations":[],"preferred":false,"id":372346,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hatcher, Patrick G.","contributorId":93625,"corporation":false,"usgs":true,"family":"Hatcher","given":"Patrick","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":372347,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lerch, H. E. 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Jr.","contributorId":19946,"corporation":false,"usgs":true,"family":"Williams","given":"Richard","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":914691,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Ferrigno, Jane G. jferrign@usgs.gov","contributorId":39825,"corporation":false,"usgs":true,"family":"Ferrigno","given":"Jane","email":"jferrign@usgs.gov","middleInitial":"G.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":914692,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Allison, Ian","contributorId":344788,"corporation":false,"usgs":false,"family":"Allison","given":"Ian","email":"","affiliations":[],"preferred":false,"id":219370,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":219371,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chinn, Trevor J.","contributorId":344745,"corporation":false,"usgs":false,"family":"Chinn","given":"Trevor","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":914690,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":17532,"text":"ofr89284 - 1989 - Preliminary geologic map of the Puu Anahulu quadrangle, Hawaii","interactions":[],"lastModifiedDate":"2022-03-25T18:46:05.283311","indexId":"ofr89284","displayToPublicDate":"1995-04-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-284","title":"Preliminary geologic map of the Puu Anahulu quadrangle, Hawaii","docAbstract":"Vent deposits and lava flows from Hualalai Volcano and lava flows from Mauna Loa and Mauna Kea Volcanoes cover the Puu Anahulu 7 1/2-minute quadrangle. Hualalai's diffuse north-trending rift zone, marked by the large trachyte cone of Puu Waawaa and several basaltic spatter cones, is located mainly in the southwestern part of the quadrangle. Several Hualalai flows originated in the Hualalai quadrangle, crossed the Puu Anahulu quadrangle, and terminated in the Kiholo quadrangle. Hualalai flows cover most of the western half of the quadrangle and are interlayered with Mauna Loa lavas along a 2-kilometer-wide strip from southeast to northwest across the middle of the Puu Anahulu quadrangle. Mauna Loa flows cover most of the eastern half. Mauna Kea flows are restricted to the northeastern corner, where they underlie Hualalai and Mauna Loa lavas. A few extensive and relatively young flows from Hualalai and Mauna Loa cover most of the quadrangle; thus, the older units are generally small in area. The oldest units in the quadrangle are the trachyte cone of Puu Waawaa and its flow, which includes Puu Anahulu, covers about 7 percent of the quadrangle. Basaltic lavas of Hualalai range in age from latest Pleistocene to less than 2,000 years. Pleistocene lavas cover about 5 percent of this quadrangle, lavas that are 5,000 - 10,000 years old cover about 5 percent, lavas that are 3,000 - 5,000 years old cover about 3 percent, and three extensive flows that are 1,500 - 3,000 years old cover about 25 percent. The oldest Mauna Loa flows, that are probably 5,000 - 10,000 years old, cover about 2 percent of this quadrangle, flows that are 3,000 - 5,000 years old cover about 18 percent, six extensive flows that are 1,500 - 3,000 years old cover about 23 percent, and the 1859 flow, that is the youngest volcanic unit, and covers about 10 percent of its area. Two hawaiite flows from Mauna Kea, that are late Pleistocene in age, cover about 2 percent of the quadrangle.
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Lambert Conformal Conic projection, https://doi.org/10.3133/a14.","productDescription":"1 Sheet, 28 x 33 inches in color; Lambert Conformal Conic projection","costCenters":[],"links":[{"id":112485,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://repository.agic.umn.edu/maps/usgs/geologic/a14_welcome_mountain/","linkFileType":{"id":5,"text":"html"}},{"id":248252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/a/14/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":248253,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/a/14/plate-1.pdf","size":"5132","linkFileType":{"id":1,"text":"pdf"}},{"id":253076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/a/14/report-thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 157.5,-73 ], [ 157.5,-72 ], [ 162,-72 ], [ 162,-73 ], [ 157.5,-73 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db64124b","contributors":{"authors":[{"text":"Stump, Edmund (compiler)","contributorId":65541,"corporation":false,"usgs":true,"family":"Stump","given":"Edmund","suffix":"(compiler)","email":"","affiliations":[],"preferred":false,"id":266849,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12527,"text":"ofr89157 - 1989 - Multichannel seismic-reflection profiles collected in 1979 aboard M/V Seismic Explorer on the western Florida shelf","interactions":[],"lastModifiedDate":"2018-06-18T10:58:09","indexId":"ofr89157","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-157","title":"Multichannel seismic-reflection profiles collected in 1979 aboard M/V Seismic Explorer on the western Florida shelf","docAbstract":"In August 1979, the U.S. Geological Survey (USGS) aboard the M/V SEISMIC EXPLORER of Seismic Explorations International (SEI), ran 17 lines (1,270 km) of multichannel, seismic-reflection profiles on the western Florida Shelf. The main features of the SEI system were (1) a digital recorder with an instantaneous-floating-point-gain constant of 24 dB, (2) a 64-channel hydrophone streamer, 3,200 m long, and (3) a 21-airgun array that had a total volume of 2,000 in and a pressure of 2,000 psi. Sampling interval was array to the center of the farthest phone group was 3,338 m and to the nearest phone group, 188 m. Shot points were 5O m apart to obtain a 32-fold stack. Navigation was by an integrated satellite/Loran/doppler-sonar system.
The SEI data were processed by Geophysical Data Processing Center, Inc. of Houston, Texas. Processing procedures were standard with the following exceptions: (1) a deringing deconvolution that had a 128-ms operator length was done prior to stacking. (2) a time-variant predictive deconvolution that had a filter operator length of 100 ms and automatic picking of the second zero-crossing was applied after stacking to further suppress multiple energy. (3) Velocity analyses were performed every 3 km, using a technique that included the determination and consideration of both the amount and direction of apparent dip. (4) Automatic gain ranging using a 750-ms window was applied pre- and post-stack. ( 5) Lines affected by sea floor's angle of slope were deconvolved again before stacking and time-variant filter parameters were adjusted to follow the sea-floor geometry.
The data taken with the 3,200-m streamer and 2,000 in3 airgun array, aboard M/V SEISMIC EXPLORER (Arabic numerals) are vastly superior to those obtained by R/V GYRE using a much smaller streamer and source (Roman numerals). The former consistently show coherent primary events from within the units underlying the Mesozoic section on the western Florida Shelf, while the latter tend to do so only in the inshore area where pre-Mesozoic basement occurs at depths of less than 2 km. The R/V GYRE data were open filed previously (Ball and others, 1987). A synthesis of both sets of data is included in Ball and others (1988).
Reflectors correlate to the full 8-s duration of recording time. A number of lines were restarted due to equipment failure; no areas were omitted, however, shotpoints overlap. The original records may be seen at the USGS branch of Atlantic marine geology offices in Woods Hole, Mass. Copies of the multichannel data may be purchased only from the National Geophysical Data Center, NOAA, Code E64, 325 Broadway, Boulder, CO 80303 (tel. 303/497-6345).
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U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89432","usgsCitation":"Blank, H.R., and Kucks, R., 1989, Preliminary aeromagnetic, gravity, and generalized geologic maps of the USGS basin and range-Colorado Plateau transit zone study area in southwestern Utah, southeastern Nevada, and northwestern Arizona (the \"BARCO\" project): U.S. Geological Survey Open-File Report 89-432, Report: 16 p.; 3 Plates: 47.00 × 35.74 inches or smaller, https://doi.org/10.3133/ofr89432.","productDescription":"Report: 16 p.; 3 Plates: 47.00 × 35.74 inches or smaller","costCenters":[],"links":[{"id":143799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0432/report-thumb.jpg"},{"id":41118,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0432/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41119,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0432/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41120,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0432/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41121,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0432/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389232,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18952.htm"}],"country":"United States","state":"Arizona, Neveda, Utah","otherGeospatial":"Colorado Plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.00,\n 36\n ],\n [\n -112.00,\n 36\n ],\n [\n -112.00,\n 38\n ],\n [\n -115.00,\n 38\n ],\n [\n -115.00,\n 36\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acae4b07f02db67ccf4","contributors":{"authors":[{"text":"Blank, H. 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During 1985, public supply, irrigation, and self-supplied industry required 38% of the 56 ,500 acre-ft of appropriated surface water and 57% of the 187 ,800 acre-ft of appropriated groundwater. If the historic (1920-80) annual population growth rate (2.8%) continues, the 126,100 acre ft of water appropriated for public-water supplies should meet demand until 2015. The quantity of potentially available water supplies was estimated by summing those resources having less than 1.00 mg/L dissolved solids. Surface water resources that meet this criterion are the Little Arkansas and Ninnescah Rivers and Cheney Reservoir. Subtracting legislated minimum streamflows for the rivers from their mean annual streamflow volumes leaves 532,000 acre-ft, which combined with the annual sustained yield of Cheney Reservoir (40,000 acre-ft) provides an estimated 572,000 acre-ft of surface water annually. Groundwater that meets the criterion was estimated by summing the annual precipitation recharge available to unconsolidated deposits in the county (78,400 acre-ft) and in the Harvey County part of the Wichita well field (13,000 acre-ft). Although more groundwater is available, withdrawals exceeding annual precipitation recharge would cause water level declines. Because less than 4% of the potentially available surface water was used for supplies in 1985 and because about 120% of the groundwater recharge was used, surface water resources have a greater potential for meeting future water use demands. (USGS)","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/ofr88711","usgsCitation":"Bevans, H.E., 1989, Water supply and demand in Sedgwick County, Kansas: U.S. Geological Survey Open-File Report 88-711, 2 p. 1 map ;28 cm., https://doi.org/10.3133/ofr88711.","productDescription":"2 p. 1 map ;28 cm.","costCenters":[],"links":[{"id":972,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://ks.water.usgs.gov/pubs/fact-sheets/ofr.88-711.bevans.html","linkFileType":{"id":5,"text":"html"}},{"id":145718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0711/report-thumb.jpg"},{"id":41094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0711/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e33df","contributors":{"authors":[{"text":"Bevans, Hugh E.","contributorId":11589,"corporation":false,"usgs":true,"family":"Bevans","given":"Hugh","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":166539,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15928,"text":"ofr89470 - 1989 - Lateral and depth variablity in chemical composition of soil at the Kendrick Reclamation Project Area, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:07:14","indexId":"ofr89470","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-470","title":"Lateral and depth variablity in chemical composition of soil at the Kendrick Reclamation Project Area, Wyoming","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr89470","usgsCitation":"Severson, R.C., Crock, J., and Erdman, J.A., 1989, Lateral and depth variablity in chemical composition of soil at the Kendrick Reclamation Project Area, Wyoming: U.S. Geological Survey Open-File Report 89-470, 27 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89470.","productDescription":"27 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":149399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0470/report-thumb.jpg"},{"id":44898,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0470/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e62","contributors":{"authors":[{"text":"Severson, R. 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A.","contributorId":59786,"corporation":false,"usgs":true,"family":"Erdman","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":171962,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":16184,"text":"ofr89309 - 1989 - Geologic maps of the French Butte and Greenhorn Buttes quadrangles, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:07:09","indexId":"ofr89309","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-309","title":"Geologic maps of the French Butte and Greenhorn Buttes quadrangles, Washington","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89309","usgsCitation":"Swanson, D., 1989, Geologic maps of the French Butte and Greenhorn Buttes quadrangles, Washington: U.S. Geological Survey Open-File Report 89-309, 25 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr89309.","productDescription":"25 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":108794,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17630.htm","linkFileType":{"id":5,"text":"html"},"description":"17630"},{"id":148562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0309/report-thumb.jpg"},{"id":45117,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0309/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45118,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0309/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45119,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0309/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45120,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0309/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2cbc","contributors":{"authors":[{"text":"Swanson, Donald A. 0000-0002-1680-3591","orcid":"https://orcid.org/0000-0002-1680-3591","contributorId":22303,"corporation":false,"usgs":true,"family":"Swanson","given":"Donald A.","affiliations":[],"preferred":false,"id":172386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18334,"text":"ofr89558 - 1989 - Spectrographic analyses of insoluble-residue samples, Joplin 1 degree x 2 degrees Quadrangle, Kansas and Missouri; drill hole Nos. 46, 47 and 48","interactions":[],"lastModifiedDate":"2012-02-02T00:07:27","indexId":"ofr89558","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-558","title":"Spectrographic analyses of insoluble-residue samples, Joplin 1 degree x 2 degrees Quadrangle, Kansas and Missouri; drill hole Nos. 46, 47 and 48","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr89558","usgsCitation":"Bullock, J.H., and Whitney, H.A., 1989, Spectrographic analyses of insoluble-residue samples, Joplin 1 degree x 2 degrees Quadrangle, Kansas and Missouri; drill hole Nos. 46, 47 and 48: U.S. Geological Survey Open-File Report 89-558, 16 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89558.","productDescription":"16 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":150835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0558/report-thumb.jpg"},{"id":47686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0558/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c9d","contributors":{"authors":[{"text":"Bullock, J. 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