Variations in sulfur mineralization in the Parachute Creek member of Green River Formation, Colorado and Utah
Conference
·
· Oil Shale Symp. Proc.; (United States)
OSTI ID:5167130
Sulfur in the Parachute Creek Member of the Green River Formation occurs primarily as pyrite, with lesser amounts of marcasite and pyrrhotite. In this study 222 samples were collected from the openlacustrine facies at Rio Blanco, the marginallacustrine facies at Douglas Pass, and a WOSCO oil shale core drilled in the Eastern Uinta Basin. One portion of each sample was crushed and analyzed for total-weight-percent sulfur (TWPS). Polished blocks were prepared from the remaining slabs. Iron-sulfide morphotypes in these blocks were characterized with a reflected light microscope. Total sulfur contents ranged from 0.0 to 4.6 wt %. Open-lacustrine oil shales in the Parachute Creek Member have much higher relative TWPS values than marginal-lacustrine rocks from the same member. In oil shale, increases in kerogen content are mirrored by increases in total-sulfur content. This correlation is most significant for moderate- to rich-grade oil shales which average between 0.42 and 0.98 TWPS. In oil shale with high relative total sulfur contents, megascopic pods and stringers and microscopic blades, compound-blade clusters and bands, and irregular massive blebs of iron sulfide are the most abundant morphotypes. Stratigraphic variations in sulfur mineralization are present at Rio Blanco. High TWPS values (more than 0.5) are found in the Mahogany ledge and R-8 zone. Rocks above and below this interval have TWPS values less than 0.5. Cyclical stratigraphic variations in TWPS values occur in the Mahogany and R-8 zones.
- Research Organization:
- ARCO Exploration Co., Denver, CO
- OSTI ID:
- 5167130
- Report Number(s):
- CONF-830434-
- Conference Information:
- Journal Name: Oil Shale Symp. Proc.; (United States)
- Country of Publication:
- United States
- Language:
- English
Similar Records
Comparative mineralogy of nearshore and offshore lacustrine lithofacies, Parachute Creek Member of the Green River Formation, Piceance Creek Basin, Colorado, and eastern Uinta Basin, Utah
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Stratigraphic variation of sulfur isotopes in Colorado Corehole Number 1
Journal Article
·
Sun Oct 01 00:00:00 EDT 1978
· Geol. Soc. Am., Bull.; (United States)
·
OSTI ID:6723408
Instrumental analysis of tars and their correlations in oil-impregnated sandstone beds, Uintah and Grand Counties, Utah
Thesis/Dissertation
·
Wed Dec 31 23:00:00 EST 1969
·
OSTI ID:6124312
Stratigraphic variation of sulfur isotopes in Colorado Corehole Number 1
Conference
·
Thu Mar 31 23:00:00 EST 1983
· Oil Shale Symp. Proc.; (United States)
·
OSTI ID:5286953
Related Subjects
04 OIL SHALES AND TAR SANDS
040201* -- Oil Shales & Tar Sands-- Site Geology-- (-1989)
BITUMINOUS MATERIALS
CARBONACEOUS MATERIALS
CHALCOGENIDES
CHEMISTRY
COLORADO
DRILL CORES
ELEMENTS
ENERGY SOURCES
FEDERAL REGION VIII
FOSSIL FUELS
FUELS
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGY
GREEN RIVER FORMATION
IRON COMPOUNDS
IRON SULFIDES
KEROGEN
MATERIALS
MINERAL RESOURCES
MINERALIZATION
MINERALOGY
NONMETALS
NORTH AMERICA
OIL SHALE DEPOSITS
OIL SHALES
ORGANIC MATTER
RESOURCES
RIO BLANCO OIL SHALE PROJECT
STRATIGRAPHY
SULFIDES
SULFUR
SULFUR COMPOUNDS
SULFUR CONTENT
TRANSITION ELEMENT COMPOUNDS
UINTA BASIN
USA
UTAH
040201* -- Oil Shales & Tar Sands-- Site Geology-- (-1989)
BITUMINOUS MATERIALS
CARBONACEOUS MATERIALS
CHALCOGENIDES
CHEMISTRY
COLORADO
DRILL CORES
ELEMENTS
ENERGY SOURCES
FEDERAL REGION VIII
FOSSIL FUELS
FUELS
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGY
GREEN RIVER FORMATION
IRON COMPOUNDS
IRON SULFIDES
KEROGEN
MATERIALS
MINERAL RESOURCES
MINERALIZATION
MINERALOGY
NONMETALS
NORTH AMERICA
OIL SHALE DEPOSITS
OIL SHALES
ORGANIC MATTER
RESOURCES
RIO BLANCO OIL SHALE PROJECT
STRATIGRAPHY
SULFIDES
SULFUR
SULFUR COMPOUNDS
SULFUR CONTENT
TRANSITION ELEMENT COMPOUNDS
UINTA BASIN
USA
UTAH