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Changes in optical properties, chemistry, and micropore and mesopore characteristics of bituminous coal at the contact with dikes in the Illinois Basin
Maria Mastalerz, A. Drobniak, A. Schimmelmann
2009, International Journal of Coal Geology (77) 310-319
Changes in high-volatile bituminous coal (Pennsylvanian) near contacts with two volcanic intrusions in Illinois were investigated with respect to optical properties, coal chemistry, and coal pore structure. Vitrinite reflectance (Ro) increases from 0.62% to 5.03% within a distance of 5.5??m from the larger dike, and from 0.63% to 3.71% within...
Martian mud volcanism: Terrestrial analogs and implications for formational scenarios
James A. Skinner, A. Mazzini
2009, Marine and Petroleum Geology (26) 1866-1878
The geology of Mars and the stratigraphic characteristics of its uppermost crust (mega-regolith) suggest that some of the pervasively-occurring pitted cones, mounds, and flows may have formed through processes akin to terrestrial mud volcanism. A comparison of terrestrial mud volcanism suggests that equivalent Martian processes likely required discrete sedimentary depocenters,...
Dike intrusions into bituminous coal, Illinois Basin: H, C, N, O isotopic responses to rapid and brief heating
A. Schimmelmann, Maria Mastalerz, L. Gao, P.E. Sauer, K. Topalov
2009, Geochimica et Cosmochimica Acta (73) 6264-6281
Unlike long-term heating in subsiding sedimentary basins, the near-instantaneous thermal maturation of sedimentary organic matter near magmatic intrusions is comparable to artificial thermal maturation in the laboratory in terms of short duration and limited extent. This study investigates chemical and H, C, N, O isotopic changes in high volatile bituminous...
Character and spatial distribution of OH/H2O on the surface of the moon seen by M3 on chandrayaan-1
C.M. Pieters, J.N. Goswami, R. N. Clark, M. Annadurai, J. Boardman, B. Buratti, J. -P. Combe, M.D. Dyar, R. Green, J.W. Head, C. Hibbitts, M. Hicks, P. Isaacson, R. Klima, G. Kramer, S. Kumar, E. Livo, S. Lundeen, E. Malaret, T. McCord, J. Mustard, J. Nettles, N. Petro, C. Runyon, M. Staid, J. Sunshine, L.A. Taylor, S. Tompkins, P. Varanasi
2009, Science (326) 568-572
The search for water on the surface of the anhydrous Moon had remained an unfulfilled quest for 40 years. However, the Moon Mineralogy Mapper (M 3) on Chandrayaan-1 has recently detected absorption features near 2.8 to 3.0 micrometers on the surface of the Moon. For silicate bodies, such features are...
A mass balance mercury budget for a mine-dominated lake: Clear Lake, California
T.H. Suchanek, J. Cooke, K. Keller, S. Jorgensen, P.J. Richerson, Collin A. Eagles-Smith, E.J. Harner, D.P. Adam
2009, Water, Air, & Soil Pollution (196) 51-73
The Sulphur Bank Mercury Mine (SBMM), active intermittently from 1873–1957 and now a USEPA Superfund site, was previously estimated to have contributed at least 100 metric tons (105 kg) of mercury (Hg) into the Clear Lake aquatic ecosystem. We have confirmed this minimum estimate. To better quantify the contribution of the...
Did the Middlesboro, Kentucky, bolide impact event influence coal rank?
J.C. Hower, S.F. Greb, K.W. Kuehn, C.F. Eble
2009, International Journal of Coal Geology (79) 92-96
The Middlesboro Basin, southeastern Kentucky, occurs on the Cumberland Overthrust Sheet and includes a ca. 5.5-km diameter impact structure. The Lower and Middle Pennsylvanian coal-bearing strata are faulted, with some evidence for shock metamorphism. The event post-dated the latest-Pennsylvanian-early-Permian thrusting and was likely prior to late-Mesozoic entrenchment of drainages. The...
Nitrogen losses from dairy manure estimated through nitrogen mass balance and chemical markers
Alexander N. Hristov, S. Zaman, M. Vander Pol, P. Ndegwa, L. Campbell, S. Silva
2009, Journal of Environmental Quality (38) 2438-2448
Ammonia is an important air and water pollutant, but the spatial variation in its concentrations presents technical difficulties in accurate determination of ammonia emissions from animal feeding operations. The objectives of this study were to investigate the relationship between ammonia volatilization and ??15N of dairy manure and the feasibility of...
Mobility of icy sand packs, with application to Martian permafrost
W. B. Durham, A.V. Pathare, L.A. Stern, H.J. Lenferink
2009, Geophysical Research Letters (36)
[1] The physical state of water on Mars has fundamental ramifications for both climatology and astrobiology. The widespread presence of "softened" Martian landforms (such as impact craters) can be attributed to viscous creep of subsurface ground ice. We present laboratory experiments designed to determine the minimum amount of ice necessary...
Organic geochemistry of resins from modern Agathis australis and Eocene resins from New Zealand: Diagenetic and taxonomic implications
P.C. Lyons, Maria Mastalerz, W. H. Orem
2009, International Journal of Coal Geology (80) 51-62
A maturation series of resins and fossil resins from New Zealand, ranging in age from Modern to Eocene and ranging from uncoalified to high volatile C bituminous coal, were analyzed by elemental, pyrolysis-gas chromatography (Py-GC), Fourier Transform infrared (FTir), and solid-state 13C nuclear magnetic resonance (13C NMR) techniques. For comparison,...
Halogen degassing during ascent and eruption of water-poor basaltic magma
M. Edmonds, T.M. Gerlach, Richard A. Herd
2009, Chemical Geology (263) 122-130
A study of volcanic gas composition and matrix glass volatile concentrations has allowed a model for halogen degassing to be formulated for K??lauea Volcano, Hawai'i. Volcanic gases emitted during 2004-2005 were characterised by a molar SO2/HCl of 10-64, with a mean of 33; and a molar HF/HCl of 0-5, with...
Improved constraints on the estimated size and volatile content of the Mount St. Helens magma system from the 2004-2008 history of dome growth and deformation
L.G. Mastin, M. Lisowski, E. Roeloffs, N. Beeler
2009, Geophysical Research Letters (36)
The history of dome growth and geodetic deflation during the 2004-2008 Mount St. Helens eruption can be fit to theoretical curves with parameters such as reservoir volume, bubble content, initial overpressure, and magma rheology, here assumed to be Newtonian viscous, with or without a solid plug in the conduit center....
Effects of megascale eruptions on Earth and Mars
T. Thordarson, M. Rampino, L. P. Keszthelyi, S. Self
2009, Special Paper of the Geological Society of America 37-53
Volcanic features are common on geologically active earthlike planets. Megascale or "super" eruptions involving >1000 Gt of magma have occurred on both Earth and Mars in the geologically recent past, introducing prodigious volumes of ash and volcanic gases into the atmosphere. Here we discuss felsic (explosive) and mafi c (flood...
Pre-1991 sulfur transfer between mafic injections and dacite magma in the Mt. Pinatubo reservoir
Muro A. Di, John S. Pallister, B. Villemant, Chris Newhall, M. Semet, M. Martinez, C. Mariet
2008, Journal of Volcanology and Geothermal Research (175) 517-540
Before the 1991–1992 activity, a large andesite lava dome belonging to the penultimate Pinatubo eruptive period (Buag ∼ 500 BP) formed the volcano summit. Buag porphyritic andesite contains abundant amphibole-bearing microgranular enclaves of basaltic–andesite composition. Buag enclaves have lower K2O and incompatible trace element (LREE,...
The roles of fractional crystallization, magma mixing, crystal mush remobilization and volatile-melt interactions in the genesis of a young basalt-peralkaline rhyolite suite, the greater Olkaria volcanic complex, Kenya Rift valley
R. Macdonald, H. E. Belkin, J.G. Fitton, N.W. Rogers, K. Nejbert, A.G. Tindle, A.S. Marshall
2008, Journal of Petrology (49) 1515-1547
The Greater Olkaria Volcanic Complex is a young (???20 ka) multi-centred lava and dome field dominated by the eruption of peralkaline rhyolites. Basaltic and trachytic magmas have been erupted peripherally to the complex and also form, with mugearites and benmoreites, an extensive suite of magmatic inclusions in the rhyolites. The...
Galileo observations of volcanic plumes on Io
P.E. Geissler, M.T. McMillan
2008, Icarus (197) 505-518
Io's volcanic plumes erupt in a dazzling variety of sizes, shapes, colors and opacities. In general, the plumes fall into two classes, representing distinct source gas temperatures. Most of the Galileo imaging observations were of the smaller, more numerous Prometheus-type plumes that are produced when hot flows of silicate lava...
Biogenic origin of coalbed gas in the northern Gulf of Mexico Coastal Plain, U.S.A
Peter D. Warwick, F. Clayton Breland Jr., Paul C. Hackley
2008, International Journal of Coal Geology (76) 119-137
New coal-gas exploration and production in northern Louisiana and south-central Mississippi, Gulf of Mexico Basin, is focused on the Wilcox Group (Paleocene–Eocene), where the depth to targeted subbituminous C to high volatile C bituminous coal beds ranges from 300 to 1680 m, and individual coal beds have a maximum thickness of...
Hydrothermal origin of halogens at Home Plate, Gusev Crater
M.E. Schmidt, S. W. Ruff, T.J. McCoy, W. H. Farrand, J. R. Johnson, Ralf Gellert, D. W. Ming, R.V. Morris, N. Cabrol, K.W. Lewis, C. Schroeder
2008, Journal of Geophysical Research E: Planets (113)
In the Inner Basin of the Columbia Hills, Gusev Crater is Home Plate, an 80 m platform of layered elastic rocks of the Barnhill class with microscopic and macroscopic textures, including a bomb sag, suggestive of a phreatomagmatic origin. We present data acquired by the Spirit Mars Exploration Rover by...
The formation conditions of chondrules and chondrites
C. M. O'D. Alexander, Jeffrey N. Grossman, D.S. Ebel, F.J. Ciesla
2008, Science (320) 1617-1619
Chondrules, which are roughly millimeter-sized silicate-rich spherules, dominate the most primitive meteorites, the chondrites. They formed as molten droplets and, judging from their abundances in chondrites, are the products of one of the most energetic processes that operated in the early inner solar system. The conditions and mechanism of chondrule...
Petrographic and Vitrinite Reflectance Analyses of a Suite of High Volatile Bituminous Coal Samples from the United States and Venezuela
Paul C. Hackley, Jonathan J. Kolak
2008, Open-File Report 2008-1230
This report presents vitrinite reflectance and detailed organic composition data for nine high volatile bituminous coal samples. These samples were selected to provide a single, internally consistent set of reflectance and composition analyses to facilitate the study of linkages among coal composition, bitumen generation during thermal maturation, and geochemical characteristics...
Natural and Human Influences on Water Quality in a Shallow Regional Unconsolidated Aquifer, Northern Atlantic Coastal Plain
Scott W. Ator
2008, Scientific Investigations Report 2008-5190
Data collected from more than 400 wells in the surficial unconfined aquifer in the Northern Atlantic Coastal Plain (New York through North Carolina) were compiled and analyzed to improve understanding of multiple natural and human influences on water quality in such shallow regional aquifers. Geochemical patterns were identified and described...
Design and Operation of a Borehole Straddle Packer for Ground-Water Sampling and Hydraulic Testing of Discrete Intervals at U.S. Air Force Plant 6, Marietta, Georgia
Owen G. Holloway, Jonathan P. Waddell
2008, Open-File Report 2008-1349
A borehole straddle packer was developed and tested by the U.S. Geological Survey to characterize the vertical distribution of contaminants, head, and hydraulic properties in open-borehole wells as part of an ongoing investigation of ground-water contamination at U.S. Air Force Plant 6 (AFP6) in Marietta, Georgia. To better understand contaminant...
Ground-water quality data in the middle Sacramento Valley study unit, 2006— Results from the California GAMA program
Stephen J. Schmitt, Miranda S. Fram, Barbara J. Milby Dawson, Kenneth Belitz
2008, Data Series 385
Ground-water quality in the approximately 3,340 mi2 Middle Sacramento Valley study unit (MSACV) was investigated from June through September, 2006, as part of the California Groundwater Ambient Monitoring and Assessment (GAMA) program. The GAMA Priority Basin Assessment project was developed in response to the Groundwater Quality Monitoring Act of 2001 and...
Ground-water quality data in the coastal Los Angeles Basin study unit, 2006: Results from the California GAMA Program
Timothy M. Mathany, Michael Land, Kenneth Belitz
2008, Data Series 387
Ground-water quality in the approximately 860 square-mile Coastal Los Angeles Basin study unit (CLAB) was investigated from June to November of 2006 as part of the Statewide Basin Assessment Project of the Ground-Water Ambient Monitoring and Assessment (GAMA) Program. The GAMA Statewide Basin Assessment was developed in response to the...
Water- and air-quality monitoring of Sweetwater Reservoir watershed, San Diego County, California — Phase one results continued, 2001-2003
Gregory O. Mendez, William T. Foreman, Andrew Morita, Michael S. Majewski
2008, Data Series 347
In 1998, the U.S. Geological Survey, in cooperation with the Sweetwater Authority, began a study to monitor water, air, and sediment at the Sweetwater and Loveland Reservoirs in San Diego County, California. The study includes regular sampling of water and air at Sweetwater Reservoir for chemical constituents, including volatile organic...
Geophysical Logs, Aquifer Tests, and Water Levels in Wells in and Near the North Penn Area 7 Superfund Site, Upper Gwynedd Township, Montgomery County, Pennsylvania, 2002-2006
Lisa A. Senior, Randall W. Conger, Philip H. Bird
2008, Scientific Investigations Report 2008-5154
Ground water in the vicinity of several industrial facilities in Upper Gwynedd Township and Lansdale Borough, Montgomery County, Pa., is contaminated with several volatile organic compounds (VOCs). The 2-square-mile area was placed on the National Priorities List as the North Penn Area 7 Superfund Site by the U.S. Environmental Protection...