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Page 2283, results 57051 - 57075

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Granulometry of pebble beach ridges in Fort Williams Point, Greenwich Island, Antarctic Peninsula; a possible result from Holocene climate fluctuations
E. Santana, J.F. Dumont
2007, Open-File Report 2007-1047-SRP-027
We present a granulometric study of emerged pebble beach ridges in the Fort Williams Point, Greenwich Island, Antarctic Peninsula. We studied 8 beach ridges from the shore up to 13.5 m above current sea level. The beach ridges are made of volcanic material from the surrounding relief, but also include...
Landscape geochemistry near mineralized areas of eastern Alaska: Chapter H in Recent U.S. Geological Survey studies in the Tintina Gold Province, Alaska, United States, and Yukon, Canada--results of a 5-year project
Bronwen Wang, Larry P. Gough, Richard B. Wanty, James G. Crock, Gregory K. Lee, Warren C. Day, Jim Vohden
2007, Scientific Investigations Report 2007-5289-H
The Pogo lode gold deposit was discovered in eastern Alaska in the early 1990s and provided the opportunity to study elemental distribution and mobility in the natural environment prior to mine development. Studying mineralized systems prior to mining allows us to compare the natural biogeochemical signature in mineralized versus nonmineralized...
Major magmatic events in Mt Meredith, Prince Charles Mountains: First evidence for early Palaeozoic syntectonic granites
N.A. Gongurov, A.A. Laiba, B.V. Beliatsky
2007, Open-File Report 2007-1047-SRP-100
Precambrian rocks at Mt Meredith underwent granulite-facies metamorphism M1. Zircon isotope dating for two orthogneisses revealed the following age signatures: 1294±3 and 957±4Ma; 1105±5 and 887±2Ma. The oldest ages could reflect the time of orthogneiss protolith crystallization and the latest age determinations date Grenvillian metamorphism. The metamorphic rocks were intruded...
Cartographic production for the Florida Shelf Habitat (FLaSH) map study: generation of surface grids, contours, and KMZ files
Lisa L. Robbins, Mark Hansen, Ellen Raabe, Paul O. Knorr, Joseph Browne
2007, Open-File Report 2007-1397
The Florida shelf represents a finite source of economic resources, including commercial and recreational fisheries, tourism, recreation, sand and gravel resources, phosphate, and freshwater reserves. Yet the basic information needed to locate resources, or to interpret and utilize existing data, comes from many sources, dates, and formats. A multi-agency effort...
Structure of the central Terror Rift, western Ross Sea, Antarctica
Jerome Hall, Terry Wilson, Stuart Henrys
2007, Open-File Report 2007-1047-SRP-108
The Terror Rift is a zone of post-middle Miocene faulting and volcanism along the western margin of the West Antarctic Rift System. A new seismic data set from NSF geophysical cruise NBP04-01, integrated with the previous dataset to provide higher spatial resolution, has been interpreted in this study in order...
Yellowstone grizzly bear investigations: Annual report of the Interagency Grizzly Bear Study Team, 2006
Charles C. Schwartz, Mark A. Haroldson, Karrie K. West, editor(s)
2007, Report
The contents of this Annual Report summarize results of monitoring and research from the 2006 field season. The report also contains a summary of nuisance grizzly bear (Ursus arctos horribilis) management actions. The Interagency Grizzly Bear Study Team (IGBST) continues to work on issues associated with counts of unduplicated females with...
USGS Tampa Bay Pilot Study
K. K. Yates, T. M. Cronin, M. Crane, M. Hansen, A. Nayeghandi, P. Swarzenski, T. Edgar, G. R. Brooks, B. Suthard, A. Hine, S. Locker, Debra A. Willard, D. Hastings, B. Flower, D. Hollander, R.A. Larson, K. Smith
2007, Report, Baywide Environmental Monitoring Report, 2002-2005
Many of the nation's estuaries have been environmentally stressed since the turn of the 20th century and will continue to be impacted in the future. Tampa Bay, one the Gulf of Mexico's largest estuaries, exemplifies the threats that our estuaries face (EPA Report 2001, Tampa Bay Estuary Program-Comprehensive Conservation and...
Geology and origin of epigenetic lode gold deposits, Tintina Gold Province, Alaska and Yukon
Richard J. Goldfarb, Erin E. Marsh, Craig J. R. Hart, John L. Mair, Marti L. Miller, Craig Johnson
Larry P. Gough, Warren C. Day, editor(s)
2007, Scientific Investigations Report 2007-5289-A
More than 50 million ounces of lode gold resources have been defined in the previous 15 years throughout accreted terranes of interior Alaska and in adjacent continental margin rocks of Yukon. The major deposits in this so-called Tintina Gold Province formed around 105 to 90 million years ago in east-central...
Surface-water, ground-water, and sediment geochemistry of epizonal and shear-hosted mineral deposits in the Tintina Gold Province--arsenic and antimony distribution and mobility: Chapter G in Recent U.S. Geological Survey studies in the Tintina Gold Province, Alaska, United States, and Yukon, Canada--results of a 5-year project
Seth H. Mueller, Richard J. Goldfarb, Philip L. Verplanck, Thomas P. Trainor, Richard F. Sanzolone, Monique Adams
Larry P. Gough, Warren C. Day, editor(s)
2007, Scientific Investigations Report 2007-5289-G
Epigenetic mineral deposits in the Tintina Gold Province are generally characterized by high concentrations of arsenic and antimony in their mineral assemblage. A total of 347 samples (ground water, surface water, and stream sediment) were collected to investigate the distribution and mobility of arsenic and antimony in the environment near...
Seismic facies and stratigraphy of the Cenozoic succession in McMurdo Sound, Antarctica: Implications for tectonic, climatic and glacial history
C.R. Fielding, J. Whittaker, S.A. Henrys, T. J. Wilson, T.R. Nash
2007, Open-File Report 2007-1047-SRP-090
A new stratigraphic model is presented for the evolution of the Cenozoic Victoria Land Basin of the West Antarctic Rift, based on integration of seismic reflection and drilling data. The Early Rift phase (?latest Eocene to Early Oligocene) comprises wedges of strata confined by early extensional faults, and which contain...
Triggering mechanism and tsunamogenic potential of the Cape Fear Slide complex, U.S. Atlantic margin
Matthew J. Hornbach, Luc L. Lavier, Carolyn D. Ruppel
2007, Geochemistry, Geophysics, Geosystems (8)
Analysis of new multibeam bathymetry data and seismic Chirp data acquired over the Cape Fear Slide complex on the U.S. Atlantic margin suggests that at least 5 major submarine slides have likely occurred there within the past 30,000 years, indicating that repetitive, large-scale mass wasting and associated tsunamis may be...
Basement and crustal structure of the Davis Sea region (East Antarctica): implications for tectonic setting and continent to oceanic boundary definition
Y.B. Guseva, G.L. Leitchenkov, V.V. Gandyukhin, S.V. Ivanov
2007, Open-File Report 2007-1047-SRP-025
This study is based on about 8400 km of MCS, magnetic and gravity data as well as 20 sonobuoys collected by the Russian Antarctic Expedition during 2003 and 2004 in the Davis Sea and adjacent areas between 80°E and 102°E. Major tectonic provinces and features are identified and mapped in...
Time, space, and composition relations among northern Nevada intrusive rocks and their metallogenic implications
E. A. duBray
2007, Geosphere (3) 381-405
Northern Nevada contains ∼360 igneous intrusions subequally distributed among three age groups: middle Tertiary, Cretaceous, and Jurassic. These intrusions are dominantly granodiorite and monzogranite, although some are more mafic. Major-oxide and trace-element compositions of intrusion age groups are remarkably similar, forming compositional arrays that are continuous, overlapping, and essentially indistinguishable....
Microstructural study of natural fractures in Cape Roberts Project 3 core, Western Ross Sea, Antarctica
C. Millan, T. Wilson, T. Paulsen
2007, Open-File Report 2007-1047-SRP-053
Microstructures in natural fractures in core recovered offshore from Cape Roberts, Ross Sea, Antarctica, provide new constraints on the relative timing of faulting and sedimentation in the Victoria Land Basin along the Transantarctic Mountain rift flank. This study characterizes the textures, fabrics and grain-scale structures from thin section analysis of...
GIS data for the Seaside, Oregon, Tsunami Pilot Study to modernize FEMA flood hazard maps
Florence L. Wong, Angie J. Venturato, Eric L. Geist
2007, Conference Paper, Proceedings of Coastal Zone '07
A Tsunami Pilot Study was conducted for the area surrounding the coastal town of Seaside, Oregon, as part of the Federal Emergency Management's (FEMA) Flood Insurance Rate Map Modernization Program (Tsunami Pilot Study Working Group, 2006). The Cascadia subduction zone extends from Cape Mendocino, California, to Vancouver Island, Canada. The...
Metamorphic conditions during formation of a metapelitic sillimanite-garnet gneiss from Clemence Massif, Prince Charles Mountains, East Antarctica
A.F. Corvino, S.D. Boger, C.J.L. Wilson
2007, Open-File Report 2007-1047-SRP-062
The pressure (P) and temperature (T) conditions during metamorphism of a metapelitic sillimanite-garnet gneiss from Clemence Massif, Antarctic Prince Charles Mountains, are estimated using mineral abundance information and petrogenetic P–T pseudosections computed in the chemical system MnO–N2O–CaO–K2O–FeO–MgO–Al2O3– SiO2–H2O–TiO2–Fe2O3 (MnNCKFMASHTO). Calculated mineral equilibria for the appropriate bulk composition predict that the observed...
The contribution of geomagnetic observatories and magnetic models to the study of secular variation and jerks in Antarctica
A. Meloni, L. Cafarella, P. De Michelis, R. Tozzi
2007, Open-File Report 2007-1047-SRP-071
Some of the most interesting features of the geomagnetic field and its time variations are displayed in polar areas. Observatory monthly means usually provide an excellent opportunity to study the temporal changes of the magnetic field at a given location. Unfortunately, on the Antarctic continent the distribution of the permanent ground- based observatories...
Tectonics of the West Antarctic rift system: new light on the history and dynamics of distributed intracontinental extension
C.S. Siddoway
2007, Open-File Report 2007-1047-KP-09
The West Antarctic rift system (WARS) is the product of multiple stages of intracontinental deformation from Jurassic to Present. The Cretaceous rifting phase accomplished >100 percent extension across the Ross Sea and central West Antarctica, and is widely perceived as a product of pure shear extension orthogonal to the Transantarctic...
Seller strategies on eBay: Does size matter?
Steven T. Anderson, Daniel Friedman, Garrett Milam, Nirvikar Singh
2007, International Journal of Electronic Business (5) 643-669
We examine seller tactics in 1177 eBay auctions. The largest volume sellers make rather homogeneous choices; smaller sellers are more heterogeneous. Some tactics, such as starting the auction with a ‘Buy it Now’ offer, appear to increase revenue. Perhaps due to intense competition, however, the overall impact of most tactics...
Aufeis accumulations in stream bottoms in arctic and subarctic environments as a possible indicator of geologic structure: Chapter F in Recent U.S. Geological Survey studies in the Tintina Gold Province, Alaska, United States, and Yukon, Canada--results of a 5-year project
Richard B. Wanty, Bronwen Wang, Jim Vohden, Warren C. Day, Larry P. Gough
Larry P. Gough, Warren C. Day, editor(s)
2007, Scientific Investigations Report 2007-5289-F
Thick accumulations of ice, called “aufeis,” form during winter along stream and river valleys in arctic and subarctic regions. In high-gradient alpine streams, aufeis forms mostly as a result of ground-water discharge into the stream channel. The ice occludes this discharge, perturbing the steady-state condition, and causing an incremental rise...
Seismic and chronostratigraphic results from SHALDRIL II, northwestern Weddell Sea
J.B. Anderson, J. Wellner, S. Wise, S. Bohaty, P. Manley, T. Smith, F. Weaver, D. Kulhanek
2007, Open-File Report 2007-1047-SRP-094
The 2006 SHALDRIL II cruise was conducted in the northwestern Weddell Sea, with primary drilling targets in the James Ross Basin. A site drilled along the northern edge of the James Ross Basin sampled either latest Eocene or earliest Oligocene deposits, providing a lower chronostratigraphic benchmark for our seismic stratigraphic...
Regional seismic stratigraphic correlations of the Ross Sea: Implications for the tectonic history of the West Antarctic Rift System
Robert C. Decesari, Christopher C. Sorlien, Bruce P. Luyendyk, Douglas S. Wilson, Louis Bartek, John Diebold, Sarah E. Hopkins
2007, Open-File Report 2007-1047-SRP-052
Using existing and new seismic reflection data, new and updated correlations of late Oligocene-early Miocene RSS-2 strata were made between the southern parts of Ross Sea basins. Previous studies documented Cretaceous extension across much of Ross Sea. We interpret that Cenozoic extension also occurred across Ross Sea. Subsidence during and...
Organic carbon stocks in permafrost-affected soils from Admiralty Bay, Antarctica
F.N.B. Simas, C.E.G.R. Schaefer, E.S. Mendonca, I.R. Silva, R.M. Santana, A.S.S. Ribeiro
2007, Open-File Report 2007-1047-SRP-076
Recent works show that organic matter accumulation in some soils from coastal Antarctica is higher than previously expected. The objective of the present work was to estimate the organic C stocks for soils from maritime Antarctica. Cryosols from subpolar desert landscapes presented the lowest organic C stocks. Ornithogenic soils are...