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Not all publications have extents, not all extents are completely accurate
Charnockites and granites of the western Adirondacks, New York, USA: A differentiated A-type suite
P.R. Whitney
1992, Precambrian Research (57) 1-19
Granitic rocks in the west-central Adirondack Highlands of New York State include both relatively homogeneous charnockitic and hornblende granitic gneisses (CG), that occur in thick stratiform bodies and elliptical domes, and heterogeneous leucogneisses (LG), that commonly are interlayered with metasedimentary rocks. Major- and trace-element geochemical analyses were obtained for 115...
The nature of Archean terrane boundaries: An example from the northern Wyoming Province
D.W. Mogk, P.A. Mueller, J. L. Wooden
1992, Precambrian Research (55) 155-168
The Archean northern Wyoming Province can be subdivided into two geologically distinct terranes, the Beartooth-Bighorn magmatic terrane (BBMT) and the Montana metasedimentary terrane (MMT). The BBMT is characterized by voluminous Late Archean (2.90-2.74 Ga) magmatic rocks (primarily tonalite, trondhjemite, and granite); metasedimentary rocks are preserved only as small, rare enclaves...
Chemistry of the subalkalic silicic obsidians
Ray MacDonald, Robert L. Smith, John E. Thomas
1992, Professional Paper 1523
Nonhydrated obsidians are quenched magmatic liquids that record in their chemical compositions details of the tectonic environment of formation and of the differentiation mechanisms that affected their subsequent evolution. This study attempts to analyze, in terms of geologic processes, the compositional variations in the subalkalic silicic obsidians (Si02≥70 percent by...
Geologic studies in Alaska by the U.S. Geological Survey, 1991
Dwight Culver Bradley, Cynthia Dusel-Bacon, editor(s)
1992, Bulletin 2041
This collection of twenty-one papers continues the annual series of U.S. Geological Survey reports on the geology of Alaska. These contributions, which include full-length Articles and shorter Geologic Notes, are grouped under two broad headings: Mineral Resource Studies (ten papers) and Geologic Framework Studies (eleven papers). Reports on mineral resources...
Mineral and energy resources of the BLM Roswell Resource Area, east-central New Mexico
Susan B. Bartsch-Winkler, editor(s)
1992, Open-File Report 92-261
The sedimentary formations of the Roswell Resource Area have significant mineral and energy resources. Some of the pre-Pennsylvanian sequences in the Northwestern Shelf of the Permian Basin are oil and gas reservoirs, and Pennsylvanian rocks in Tucumcari basin are reservoirs of oil and gas as well as source rocks for...
The storm and flood of September 15, 1989, in Fayetteville, North Carolina
R.R. Mason Jr., W.S. Caldwell
1992, Water-Resources Investigations Report 92-4097
The storm of September 15, 1989, in and around the city of Fayetteville, North Carolina, produced the most extensive flooding of Fayetteville since 1945. The flood inundated 925 acres in the city along Cross Creek and Blounts Creek and their tributaries, flooded 338 buildings, caused damages in excess of $10...
Assessment of nonpoint-source contamination of the High Plains Aquifer in south-central Kansas, 1987
John O. Helgesen, Lloyd E. Stullken, A. T. Rutledge
1992, Open-File Report 91-238
Ground-water quality was assessed in a 5,000-square-mile area of the High Plains aquifer in south-central Kansas that is susceptible to nonpoint-source contamination from agricultural and petroleum-production activities. Of particular interest were agricultural chemicals, mainly atrazine, and oil-derived hydrocarbons, which might occur in association with brines that formerly were disposed into...
Geology and mineral paragenesis of the Pea Ridge iron ore mine, Washington County, Missouri: Origin of the rare-earth-element- and gold-bearing breccia pipes. Some mineralogical and geochemical aspects of middle and upper Pennsylvanian marine black shales in part of the midcontinent region. Mineralogical and geochemical analysis of the metal- and organic-rich Grassy Creek Shale of the New Albany group (Upper Devonian and Lower Mississippian) in Hardin County, southern Illinois
L. M. Nuelle, Warren C. Day, Gary B. Sidder, Cheryl M. Seeger, George A. Desborough, Joseph R. Hatch, Joel S. Leventhal
Warren C. Day, Diane E. Lane, editor(s)
1992, Bulletin 1989-A-C
No abstract available....
Deep-water facies of the Lisburne Group, west-central Brooks Range, Alaska
Julie A. Dumoulin, Anita G. Harris, Jeanine M. Schmidt
Dennis K. Thurston, Kazuya Fujita, editor(s)
1992, Conference Paper, Proceedings: 1992 international conference on Arctic margins (MMS 94-0040)
Deep-water lithofacies of the Lisburne Group (chiefly Carboniferous) occur in thurst sheets in the western part of the foreland fold-and-thrust belt of the Brooks Range and represent at least three discrete units. The Kuna Formation (Brooks Range allochthon) consists mostly of spiculitic mudstone and lesser shale; subordinate carbonate layers are...
Rare earth, major and trace element composition of Leg 127 sediments
R.W. Murray, Marilyn R. Buchholtz ten Brink, Hans-Juergen Brumsack, David C. Gerlach, G. Price Russ
1992, Conference Paper, Proceedings of the Ocean Drilling Program, Scientific Results
The relative effects of paleoceanographic and paleogeographic variations, sediment lithology, and diagenetic processes on the final preserved chemistry of Japan Sea sediments are evaluated by investigating the rare earth element (REE), major element, and trace element concentrations in 59 squeeze-cake whole-round and 27 physical-property sample residues from Sites 794, 795,...
Diagenetic formation of bedded chert: Evidence from chemistry of the chert-shale couplet
Richard L. Murray, David L. Jones, Marilyn R. Buchholtz ten Brink
1992, Geology (20) 271-274
Theories concerning the formation of bedded chert traditionally have emphasized either depositional or diagenetic processes. Major and rare earth element data from Franciscan assemblage (Mesozoic) and Claremont Formation (Miocene) bedded chert sequences, along with physical observations such as the presence of rare and highly corroded radiolarians in shale interbeds, are...
Interoceanic variation in the rare earth, major, and trace element depositional chemistry of chert: Perspectives gained from the DSDP and ODP record
R.W. Murray, Marilyn R. Buchholtz ten Brink, David C. Gerlach, G. Price Russ, David L. Jones
1992, Geochimica et Cosmochimica Acta (56) 1897-1913
Rare earth element (REE), major, and trace element abundances and relative fractionations in forty nodular cherts sampled by the Deep Sea Drilling Project (DSDP) and Ocean Drilling Program (ODP) indicate that the REE composition of chert records the interplay between terrigenous sources and scavenging from the local seawater. Major and...
Rare earth, major, and trace element composition of Monterey and DSDP chert and associated host sediment: Assessing the influence of chemical fractionation during diagenesis
R.W. Murray, Marilyn R. Buchholtz ten Brink, David C. Gerlach, G. Price Russ, David L. Jones
1992, Geochimica et Cosmochimica Acta (56) 2657-2671
Chert and associated host sediments from Monterey Formation and Deep Sea Drilling Project (DSDP) sequences were analyzed in order to assess chemical behavior during diagenesis of biogenic sediments. The primary compositional contrast between chert and host sediment is a greater absolute SiO2 concentration in chert, often with final SiO2 ≥ 98 wt%....
Formation of harzburgite by pervasive melt/rock reaction in the upper mantle
P.B. Kelemen, H.J.B. Dick, J. E. Quick
1992, Nature (358) 635-641
Many mantle peridotite samples are too rich in SiO2 (in the form of orthopyroxene) and have ratios of light to heavy rare earth elements that are too high to be consistent with an origin as the residuum of partial melting of the primitive mantle. Trace element studies of melt/rock reaction...
Post-rifting stress relaxation at the divergent plate boundary in northeast Iceland
G.R. Foulger, C.-H. Jahn, G. Seeber, P. Einarsson, B.R. Julian, K. Heki
1992, Nature (358) 488-490
Interaction of the elastic lithosphere with the underlying anelastic asthenosphere causes strain to propagate along the Earth's surface in a diffusion-like manner following tectonism at plate boundaries. This process transfers stress between adjacent tectonic segments and influences the temporal tectonic pattern along a plate boundary. Observations of such strain transients...
Aluminum in soil solutions from a subalpine spruce-fir forest at Whiteface Mountain, New York
E. K. Miller, Thomas G. Huntington, A. H. Johnson, A. J. Friedland
1992, Journal of Environmental Quality (21) 345-352
Direct or indirect Al toxicity has been suggested as a principal factor in forest tree declines. We monitored ambient soil solutions in undisturbed and experimentally manipulated soils from a fir [Abies balsamea (L.) Mill.]-spruce forest on Whiteface Mountain, NY, in order to characterize soil solution Al concentrations over a range of...
Evaluation of aerial transects for counting winter mallards
Kenneth J. Reinecke, Michael W. Brown, James R. Nassar
1992, Journal of Wildlife Management (56) 515-525
Winter waterfowl surveys rarely use sampling methods, and little is known about the precision and biases of their population estimates. Consequently, we developed aerial transect surveys (n=5) in 4 strata comprising 16 substrata in the lower Mississippi Alluvial Valley during winters 1987-88 through 1989-90 to estimate mallard (Anas platyrhynchos) population...
Feeding flights of breeding double-crested cormorants at two Wisconsin colonies
T. W. Custer, C. Bunck
1992, Journal of Field Ornithology (63) 203-211
Unmarked Double-crested Cormorants (Phalacrocorax auritus) (n = 523) were followed by airplane from Cat Island and Spider Island, two nesting colonies in Wisconsin, to their first landing site. Cormorants flew an average of 2.0 km from Cat Island (maximum 40 km) and 2.4 km from Spider Island (maximum12 km)....
Petrology of the Caribou Mountain Pluton, Klamath Mountains, California
Calvin G. Barnes, Melanie Barnes, Ronald W. Kistler
1992, Journal of Petrology (33) 95-124
The Caribou Mountain pluton is a small trondhjemitic body that intruded semipelitic schist of the Stuart Fork terrane in late Middle Jurassic to Early Cretaceous time. Its emplacement followed the intrusion of an adjoining body of hornblende quartz diorite called the Middle Fork pluton and the mode of its...
Alleghanian development of the Goat Rock fault zone, southernmost Appalachians: Temporal compatibility with the master decollement
Mark G. Steltenpohl, S. Goldberg, T.B. Hanley, Michael J. Kunk
1992, Geology (20) 845-848
The Goat Rock and associated Bartletts Ferry fault zones, which mark the eastern margin of the Pine Mountain Grenville basement massif, are controversial due to the suggestion that they are rare exposed segments of the late Paleozoic southern Appalachian master decollement. The controversy in part stems from reported middle Paleozoic...
Changes in Alaskan soft-bottom prey communities along a gradient in sea otter predation
R.G. Kvitek, J.S. Oliver, A.R. DeGange, B.S. Anderson
1992, Ecology (73) 413-428
Sea Otter (Enhydra lutris), well documented as "keystone" predators in rocky marine communities, were found to exert a strong influence on infaunal prey communities in soft-sediment habitats. Direct and indirect effects of sea otter predation on subtidal soft-bottom prey communities were evaluated along a temporal gradient of sea otter occupancy...
A critical review of inductively coupled plasma-mass spectrometry for geoanalysis, geochemistry and hydrology, Part 1. Analytical performance
I.B. Brenner, Howard E. Taylor
1992, Critical Reviews in Analytical Chemistry (23) 355-367
Present-day inductively coupled plasma-mass spectrometry (ICP-MS) instrumentation is described briefly. Emphasis is placed on performance characteristics for geoanalysis, geochemistry, and hydrology. Applications where ICP-MS would be indispensable are indicated. Determination of geochemically diagnostic trace elements (such as the rare earth elements [REE], U and Th), of isotope ratios for fingerprinting,...
Decomposition techniques
T. T. Chao, R. F. Sanzolone
1992, Journal of Geochemical Exploration (44) 65-106
Sample decomposition is a fundamental and integral step in the procedure of geochemical analysis. It is often the limiting factor to sample throughput, especially with the recent application of the fast and modern multi-element measurement instrumentation. The complexity of geological materials...