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Not all publications have extents, not all extents are completely accurate
Hydrothermal alteration mineralogy of SOH drill holes, Kilauea East Rift Zone geothermal area, Hawaii
Keith E. Bargar, Terry E.C. Keith, Frank A. Trusdell, S.R. Evans, M.L. Sykes
1996, Open-File Report 96-10
Thirty-eight hydrothermal minerals were identified from 356 drill-core specimens that were obtained from three Scientific Observation Holes (SOH-1, SOH-2, and SOH-4) drilled along the lower East Rift Zone (ERZ) of Kilauea Volcano, Hawaii. The minerals formed during alteration of basaltic rocks and glass by hot, circulating, waters in aquifers consisting...
Geochemical data of fumarolically altered rocks, Valley of Ten Thousand Smokes, Alaska
Terry E. Keith
1995, Open-File Report 95-47
Samples from a fossil fumarole originating in the 1912 ash-flow tuffin the Valley of Ten Thousand Smokes have been analyzed to ascertain chemical changes resulting from high-temperature fumarolic alteration and subsequent cooling and weathering of the protolith. Samples of the underlying, dominantly leached, dacite-rich portion of the ash-flow tuff adjacent...
Fluid-inclusion evidence for past temperature fluctuations in the Kilauea East Rift Zone geothermal area, Hawaii
Keith E. Bargar, Terry E.C. Keith, Frank A. Trusdell
1995, Geothermics (24) 639-659
Heating and freezing data were obtained for fluid inclusions in hydrothermal quartz, calcite, and anhydrite from several depths in three scientific observation holes drilled along the lower East Rift Zone of Kilauea volcano, Hawaii. Compositions of the inclusion fluids range from dilute meteoric water to highly modified sea water concentrated...
Release strategies for rehabilitated sea otters
Anthony R. DeGange, Brenda E. Ballachey, Keith Bayha
Terrie M. Williams, Randall W. Davis, editor(s)
1995, Book chapter, Emergency care and rehabilitation of oiled sea otters: A guide for oil spils involving fur-bearing marine mammals
According to the U.S. Fish and Wildlife Services’ (USFWS) Response Plan for sea otters (USFWS, in preparation), in the event of an oil spill, the decision to release sea otters from rehabilitation centers following treatment will be linked to the decision on whether to capture sea otters for treatment. Assuming...
Maps showing isotopic composition of methane in seawater of the Alaskan Beaufort Sea, 1994
Thomas D. Lorenson, Keith A. Kvenvolden, Peter W. Barnes, Brian N. Popp, Frank J. Sansone, Terri M. Rust, Marvin D. Lilley, Eric J. Olson
1995, Open-File Report 95-669
We are engaged in a five-year study to test the hypothesis that methane from decomposing gas hydrates may contribute methane to the atmosphere. The release of methane, a "greenhouse" gas, can enhance global warming and be a factor in global climate change. As part of the study we have measured the...
A survey of molecular marker compounds in sediments of San Francisco Bay, California
Frances D. Hostettler, John B. Rapp, Wilfred E. Geological Survey Pereira, Keith A. Kvenvolden
1994, Conference Paper, U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993, Water-Resources Investigations Report 94-4015
An areal survey of surficial sediments in San Francisco Bay has been conducted to evaluate the presence of extractable organic compounds. Molecular marker compounds studied include hydrocarbons (PAH's), chlorinated pesticides, and other organic compounds that provide information on sources of organic input into the Bay. Fairly uniform source profiles are...
Laboratory simulation of hydrothermal petroleum formation from sediment in Escanaba Trough, offshore from northern California
Keith A. Kvenvolden, John B. Rapp, Frances D. Hostettler, Robert J. Rosenbauer
1994, Organic Geochemistry (22) 935-945
Petroleum associated with sulfide-rich sediment is present in Escanaba Trough at the southern end of the Gorda Ridge spreading axis offshore from northern California within the Exclusive Economic Zone (EEZ) of the U.S. This location and occurrence are important for evaluation of the mineral and energy resource potential of the...
Biomarkers in Tertiary mélange, western Olympic Peninsula, Washington, U.S.A.
Keith A. Kvenvolden, Frances D. Hostettler, John B. Rapp, Parke D. Snavely Jr.
1991, Chemical Geology (93) 101-110
Middle Eocene to middle Miocene mélange and broken formations are exposed in the coastal outcrops along the west side of the Olympic Peninsula, Washington. A petroleum geochemical assessment of these geologic units has included the investigation of biomarker compounds. A comparison was made of biomarkers in an oil sample from...
Hydrocarbons in sediment of the Weddell Sea, Antarctica
Keith A. Kvenvolden, Frances D. Hostettler, Tamara Frank
1990, Proceedings of the Ocean Drilling Program: Scientific Results (113) 199-208
Heavy hydrocarbons (about C15+) are ubiquitous but minor components in sediment from three sites (692, 693, and 694) drilled during Ocean Drilling Program (ODP) Leg 113. This preliminary report is the first to describe the distribution of some of these hydrocarbons in sediment of the Weddell Sea. Samples from Sites...
Hydrothermally derived petroleum: examples from Guaymas Basin, Gulf of California, and Escanaba Trough, northeast Pacific Ocean
Keith A. Kvenvolden, B.R. Simoneit
1990, AAPG Bulletin (74) 223-237
In the Guaymas Basin, a spreading axis in the Gulf of California, petroleum having a wide range of compositions forms by hydrothermal alteration of organic matter in Quaternary sediment composed mainly of marine diatomaceous ooze and muddy turbidites. In Escanaba Trough, at the southern end of the Gorda Ridge spreading...
The Geology and Remarkable Thermal Activity of Norris Geyser Basin, Yellowstone National Park, Wyoming
Donald Edward White, Roderick A. Hutchinson, Terry E.C. Keith
1988, Professional Paper 1456
Norris Geyser Basin, normally shortened to Norris Basin, is adjacent to the north rim of the Yellowstone caldera at the common intersection of the caldera rim and the Norris-Mammoth Corridor, a zone of faults, volcanic vents, and thermal activity that strikes north from the caldera rim to Mammoth Hot Springs....
Hydrothermal alteration patterns in the Breitenbush Hot Springs area, Cascade Range, Oregon
Terry E.C. Keith
1988, Conference Paper, Transactions - Geothermal Resources Council
Rocks of early Miocene age in the Breitenbush Hot Springs area have been affected by at least two major episodes of hydrothermal alteration, one of which had temperatures in excess of 200??C. Alteration minerals in younger Tertiary rocks are characteristic of temperatures below 100??C. The most important factor in controlling...
Multiple sources of alkanes in Quaternary oceanic sediment of Antarctica
Keith A. Kvenvolden, John B. Rapp, Margaret Golan-Bac, Frances D. Hostettler
1987, Organic Geochemistry (11) 291-302
Normal alkanes (n-C13n-C36), isoprenoid hydrocarbons (i-C15, i-C16, i-C18, i-C19, and i-C20) triterpanes (C27C32), and (C27C29) are present in low concentrations offshore Antarctica in near-surface, Quaternary sediment of the Wilkes Land continental margin and of the western Ross Sea. The distributions of these...
WATER CHEMISTRY AND MINERALOGY OF MORGAN AND GROWLER HOT SPRINGS, LASSEN KGRA, CALIFORNIA.
J. Michael Thompson, Terry E.C. Keith, Jerry J. Consul
1985, Conference Paper, Transactions - Geothermal Resources Council
Because these springs contain substantial amounts of dissolved chloride, halite and sylvite are found above the water level as evaporitic deposits, along with gypsum. One spring is depositing pyrite that contains significant amounts of arsenic, antimony, and thallium. A yellow compound, composed of arsenic and sulfur, is being deposited in...
Zeolites in Eocene basaltic pillow lavas of the Siletz River Volcanics, Central Coast Range, Oregon
Terry E.C. Keith, Lloyd W. Staplese
1985, Clays and Clay Minerals (33) 135-144
Zeolites and associated minerals occur in a tholeiitic basaltic pillow lava sequence that makes up part of the Eocene Siletz River Volcanics in the central Coast Range, Oregon. Regional zoning of zeolite assemblages is not apparent; the zeolites formed in joints, fractures, and interstices, although most occur in central cavities...
MINERALOGICAL STUDIES OF THE HYDROTHERMAL SYSTEM IN NEWBERRY VOLCANO DRILL HOLE 2, OREGON.
Terry E.C. Keith, Keith E. Bargar, Stephen S. Howe, William W. Carothers, Ivan Barnes
1984, Conference Paper, Transactions - Geothermal Resources Council
Studies of secondary mineral distribution, whole-rock chemical compositions, isotopes, and fluid inclusions are being conducted on the core from Newberry Volcano drill hole 2. Rocks from the drill core are divided into 3 major intervals on the basis of their alteration pattern, which is controlled by rock permeabilities, primary lithologies,...