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Cenozoic Antarctic DiatomWare/BugCam: An aid for research and teaching
S.W. Wise, M. Olney, J.M. Covington, V.M. Egerton, S. Jiang, D.K. Ramdeen, Kulhanek S., H. Schrader, P.A. Sims, A.S. Wood, A. Davis, D.R. Davenport, N. Doepler, W. Falcon, C. Lopez, T. Pressley, O.L. Swedberg, D.M. Harwood
2007, Open-File Report 2007-1047-SRP-017
Cenozoic Antarctic DiatomWare/BugCam© is an interactive, icon-driven digital-image database/software package that displays over 500 illustrated Cenozoic Antarctic diatom taxa along with original descriptions (including over 100 generic and 20 family-group descriptions). This digital catalog is designed primarily for use by micropaleontologists working in the field (at sea or on the...
Tectonic setting and metallogenesis of volcanogenic massive sulfide deposits in the Bonnifield Mining District, Northern Alaska Range: Chapter B in Recent U.S. Geological Survey studies in the Tintina Gold Province, Alaska, United States, and Yukon, Canada--results of a 5-year project
Cynthia Dusel-Bacon, John N. Aleinikoff, Wayne R. Premo, Suzanne Paradis, Ilana Lohr-Schmidt
Larry P. Gough, Warren C. Day, editor(s)
2007, Scientific Investigations Report 2007-5289-B
This paper summarizes the results of field and laboratory investigations, including whole-rock geochemistry and radiogenic isotopes, of outcrop and drill core samples from volcanogenic massive sulfide (VMS) deposits and associated metaigneous rocks in the Wood River area of the Bonnifield mining district, northern Alaska Range (see fig. 1 of Editors’...
Differences in ice retreat across Pine Island Bay, West Antarctica, since the Last Glacial Maximum: Indications from multichannel seismic reflection data
G. Uenzelmann-Neben, K. Gohl, R.D. Larter, P. Schluter
2007, Open-File Report 2007-1047-SRP-084
An understanding of the glacial history of Pine Island Bay (PIB) is essential for refining models of the future stability of the West Antarctic Ice Sheet (WAIS). New multichannel seismic reflection data from inner PIB are interpreted in context of previously published reconstructions for the retreat history in this area...
Early Precambrian mantle derived rocks in the southern Prince Charles Mountains, East Antarctica: age and isotopic constraints
E.V. Mikhalsky, F. Henjes-Kunst, N.W. Roland
2007, Open-File Report 2007-1047-SRP-039
Mafic and ultramafic rocks occurring as lenses, boudins, and tectonic slabs within metamorphic units in the southern Mawson Escarpment display mantle characteristics of either a highly enriched, or highly depleted nature. Fractionation of these mantle rocks from their sources may be as old as Eoarchaean (ca 3850 Ma) while their...
Mapping known and potential mineral occurrences and host rocks in the Bonnifield Mining District using minimal cloud- and snow-cover ASTER data: Chapter E in Recent U.S. Geological Survey studies in the Tintina Gold Province, Alaska, United States, and Yukon, Canada--results of a 5-year project
Bernard E. Hubbard, Cynthia Dusel-Bacon, Lawrence C. Rowan, Robert G. Eppinger
Larry P. Gough, Warren C. Day, editor(s)
2007, Scientific Investigations Report 2007-5289-E
On July 8, 2003, the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) sensor acquired satellite imagery of a 60-kilometer-wide swath covering a portion of the Bonnifield mining district within the southernmost part of the Tintina Gold Province, Alaska, under unusually favorable conditions of minimal cloud and snow cover. Although...
Jurassic magmatism in Dronning Maud Land: synthesis of results of the MAMOG project
P.T. Leat, M.L. Curtis, T.R. Riley, Fausto Ferraccioli
2007, Open-File Report 2007-1047-SRP-033
The Jurassic Karoo large igneous province (LIP) of Antarctica, and its conjugate margin in southern Africa, is critical for investigating important questions about the relationship of basaltic LIPs to mantle plumes. Detailed aerogeophysical, structural, anisotropy of magnetic susceptibility (AMS), geochronological and geochemical investigations completed under the British Antarctic Survey’s MAMOG...
Denudation and uplift of the Mawson Escarpment (eastern Lambert Graben, Antarctica) as indicated by apatite fission track data and geomorphological observation
F. Lisker, H. Gibson, C. J. Wilson, A. Laufer
2007, Open-File Report 2007-1047-SRP-105
Analysis of three vertical profiles from the southern Mawson Escarpment (Lambert Graben) reveals apatite fission track (AFT) ages ranging from 102±20 to 287±23 Ma and mean lengths of 12.2 to 13.0 μm. Quantitative thermal histories derived from these data consistently indicate onset of slow cooling below 110°C began sometime prior...
Multiple shallow level sill intrusions coupled with hydromagmatic explosive eruptions marked the initial phase of Ferrar large igneous province magmatism in northern Victoria Land, Antarctica
L. Viereck-Goette, R. Schoner, B. Bomfleur, J. Schneider
2007, Open-File Report 2007-1047-SRP-104
Field data gathered during GANOVEX IX (2005/2006) in Northern Victoria Land, Antarctica, indicate that volcaniclastic deposits of phreatomagmatic eruptions (so-called Exposure Hill Type events) are intercalated with fluvial deposits of Triassic-Jurassic age at two stratigraphic levels. Abundant scoriaceous spatter (locally welded) indicates a hawaiian/strombolian component. Breccia-filled diatremes, from which volcaniclastic...
Unconsolidated sediments at the bottom of Lake Vostok from seismic data
I. Filina, V. Lukin, Valery Masolov, D. Blankenship
2007, Open-File Report 2007-1047-SRP-031
Seismic soundings of Lake Vostok have been performed by the Polar Marine Geological Research Expedition in collaboration with the Russian Antarctic Expedition since the early 1990s. The seismograms recorded show at least two relatively closely spaced reflections associated with the lake bottom. These were initially interpreted as boundaries of a...
Morphotectonic architecture of the Transantarctic Mountains rift flank between the Royal Society Range and the Churchill Mountains based on geomorphic analysis
Elizabeth Demyanick, Terry J. Wilson
2007, Open-File Report 2007-1047-SRP-096
Extensional forces within the Antarctic Plate have produced the Transantarctic Mountains rift-flank uplift along the West Antarctic rift margin. Large-scale linear morphologic features within the mountains are controlled by bedrock structure and can be recognized and mapped from satellite imagery and digital elevation models (DEMs). This study employed the Antarctic...
Insight into the geology of the East Antarctic hinterland: a study of sediment inclusions from ice cores of the Lake Vostok borehole
G.L. Leitchenkov, B.V. Belyatsky, N.V. Rodionov, S.A. Sergeev
2007, Open-File Report 2007-1047-SRP-014
The borehole at the southern part of subglacial Lake Vostok has been drilled into an ice layer that has been refrozen from the lake water. This ice layer contains random sediment inclusions, eight of which have been studied using state-of the-art analytical techniques. Six inclusions comprise soft aggregates consisting mainly of...
Management applications of lidar-derived mean high water shorelines in North Carolina
Patrick W. Limber, Jeffrey H. List, Jeffrey D. Warren
2007, Conference Paper, Proceedings of Coastal Zone '07
The accuracy of shoreline change analysis is dependent on how the shoreline is defined and the consistency of the techniques(s) used to define it. Using the concurrent lidar (light detection and ranging) and orthophotography dataset from August and September of 2004 covering North Carolina's 516 kilometers of barrier island oceanfront,...
Geology of the Byrd Glacier Discontinuity (Ross Orogen): New survey data from the Britannia Range, Antarctica
R. Carosi, F. Giacomini, F. Talarico, E. Stump
2007, Open-File Report 2007-1047-SRP-030
Field activities in the Britannia Range (Transantarctic Mountains, Antarctica) highlighted new geological features around the so-called Byrd Glacier discontinuity. Recent field surveys revealed the occurrence of significant amounts of medium- to high-grade metamorphic rocks, intruded by abundant coarse-grained porphyritic granitoids. Most of the granitoids are deformed, with foliation parallel to...
Observations related to tetrahydrofuran and methane hydrates for laboratory studies of hydrate-bearing sediments
J.Y. Lee, T.S. Yun, J.C. Santamarina, C. Ruppel
2007, Geochemistry, Geophysics, Geosystems (8)
The interaction among water molecules, guest gas molecules, salts, and mineral particles determines the nucleation and growth behavior of gas hydrates in natural sediments. Hydrate of tetrahydrofuran (THF) has long been used for laboratory studies of gas hydrate-bearing sediments to provide close control on hydrate concentrations and to overcome the...
Break-up of Gondwana and opening of the South Atlantic: Review of existing plate tectonic models
M.E. Ghidella, L.A. Lawver, L.M. Gahagan
2007, Open-File Report 2007-1047-SRP-055
The opening history of both the Weddell Sea and South Atlantic Ocean is critical to understanding the break- up of Gondwana and the evolution of Antarctica since Early Jurassic times. The dispersal of the Gondwanide fragments is important to understanding the development of past ocean circulation. Unfortunately the tectonics of the Weddell...
Solubility of TiO2 in garnet and orthopyroxene: Ti thermometer for ultrahigh-temperature granulites
Toshisuke Kawasaki, Yoichi Motoyoshi
2007, Open-File Report 2007-1047-SRP-038
We report the TiO2 solubility in garnet and orthopyroxene coexisting with rutile calibrated from experimental data at pressures 7–20 kbar and temperatures 850–1300°C in two Antarctic granulite systems.The Ti would substitute for the tetrahedral Si, whereas we could not find positive evidence of the coupled substitution of M-Ti (M is...
Sea ice concentration temporal variability over the Weddell Sea and its relationship with tropical sea surface temperature
S. Barreira, R. Compagnucci
2007, Open-File Report 2007-1047-SRP-029
Principal Components Analysis (PCA) in S-Mode (correlation between temporal series) was performed on sea ice monthly anomalies, in order to investigate which are the main temporal patterns, where are the homogenous areas located and how are they related to the sea surface temperature (SST). This analysis provides 9 patterns (4...
SCIAMACHY’s View of the Polar Atmosphere
M. Gottwald, E. Krieg, C. von Savigny, S. Noel, A. Reichl, H. Bovensmann, J.P. Burrows
2007, Open-File Report 2007-1047-SRP-011
The instrument SCIAMACHY onboard the European ENVISAT mission provides unique capabilities for deriving atmospheric geophysical parameters. Since its launch in early 2002 it has operated successfully in orbit. Due to ENVISAT’s high inclination orbit the polar regions are monitored continuously. We report here results about the status of the polar...
Crustal structure and evolution of the Mawson Sea, western Wilkes Land margin, East Antarctica
G.L. Leitchenkov, V.V. Gandyukhin, Yu. B. Guseva, A. Yu Kazankov
2007, Open-File Report 2007-1047-SRP-028
Thisstudy is based on about 4000 km of MCS, magnetic and gravity data as well as 10 sonobuoys collected by the 2005 Russian Antarctic Expedition in the Mawson Sea and adjacent Australian-Antarctic basin between 102°E and 115°E. Major identified tectonic provinces and features of the study region include: 1) A marginal...
East Antarctic Ice Sheet fluctuations during the Middle Miocene Climatic Transition inferred from faunal and biogeochemical data on planktonic foraminifera (ODP Hole 747A, Kerguelen Plateau)
M. Verducci, L.M. Foresi, G.H. Scott, Tiepolo, M. Sprovieri, F. Lirer
2007, Open-File Report 2007-1047-SRP-037
This research focuses on a detailed study of faunal and biogeochemical changes that occurred at ODP Hole 747A in the Kerguelen Plateau region of the Southern Ocean during the middle Miocene (14.8-11.8 Ma). Abundance fluctuations of several planktonic foraminiferal taxa, stable oxygen isotope and Mg/Ca ratios have been integrated as...
Thermochronologic constraints on the tectonic evolution of the western Antarctic Peninsula in late Mesozoic and Cenozoic times
M.R. Brix, V. Faundez, F. Herve, M. Solari, J. Fernandez, A. Carter, B. Stockhert
2007, Open-File Report 2007-1047-SRP-101
West of the Antarctic Peninsula, oceanic lithosphere of the Phoenix plate has been subducted below the Antarctic plate. Subduction has ceased successively from south to north over the last 65 Myr. An influence of this evolution on the segmentation of the crust in the Antarctic plate is disputed. Opposing scenarios...
Modeling environmental bias and computing velocity field from data of Terra Nova Bay GPS network in Antarctica by means of a quasi-observation processing approach
Giuseppe Casula, Marco Dubbini, Angelo Galeandro
2007, Open-File Report 2007-1047-SRP-054
A semi-permanent GPS network of about 30 vertices has been installed at Terra Nova Bay (TNB) near Ross Sea in Antarctica. A permanent GPS station TNB1 based on an Ashtech Z-XII dual frequency P-code GPS receiver with ASH700936D_M Choke Ring Antenna has been mounted on a reinforced concrete pillar built...
Crustal architecture of the oblique-slip conjugate margins of George V Land and southeast Australia
H.M.J. Stagg, A.M. Reading
2007, Open-File Report 2007-1047-SRP-109
A conceptual, lithospheric-scale cross-section of the conjugate, oblique-slip margins of George V Land, East Antarctica, and southeast Australia (Otway Basin) has been constructed based on the integration of seismic and sample data. This cross-section is characterised by asymmetry in width and thickness, and depth-dependent crustal extension at breakup in the...
Survey report of NOAA Ship McArthur II cruises AR-04-04, AR-05-05 and AR-06-03: habitat classification of side scan sonar imagery in support of deep-sea coral/sponge explorations at the Olympic Coast National Marine Sanctuary
Steven S. Intelmann, Guy R. Cochrane, C. Edward Bowlby, Mary Sue Brancato, Jeffrey Hyland
2007, Report
Habitat mapping and characterization has been defined as a high-priority management issue for the Olympic Coast National Marine Sanctuary (OCNMS), especially for poorly known deep-sea habitats that may be sensitive to anthropogenic disturbance. As a result, a team of scientists from OCNMS, National Centers for Coastal Ocean Science (NCCOS), and...