Organic geochemical and tectonic evolution of the midcontinent rift system: Organic geochemistry and micropaleontology
Technical Report
·
OSTI ID:5628359
- Indiana Univ., Bloomington, IN (USA)
Siltstones and shales of the mid-Proterozoic Nonesuch Formation are widely postulated to be effective petroleum source rocks based on the occurrence of active oil seeps and tarry residues within parts of the Copper Range Mine. Most previous organic geochemical research has focused on mineralized sedimentary strata and associated oils in the lower-most 5 meters of the Nonesuch Formation exposed in mine excavations. Recently, non-mineralized sediments from outcrops along the shore of Lake Michigan and exploration cores drilled along the subsurface trend to the east of White Pine have been studied. Substantial variation in the lateral and vertical distribution of fine-grained facies within the Nonesuch is apparent from our studies of the non-mineralized suites of samples. Research at Indiana University is focused on the relationship between organic geochemistry and depositional environment in the Nonesuch Formation. Our principal objectives are (1) to describe the distribution of fine-grained lithofacies; (2) to determine organic-carbon, carbonate-carbon, and total-sulfur contents of these units; (3) to characterize the extractable bitumen and conduct preliminary analyses of selected biomarkers (hopanoids, steroids, and monomethyl-substituted cyclohexyl alkanes); and (4) to infer the depositional environment and biological affinities of organic matter preserved in the Nonesuch. These data will be used to evaluate the regional source-rock potential of the Nonesuch Formation. A parallel study of sedimentary structures, petrography, and organic geochemistry of the slightly older Belt Group in Montana will provide a context for interpretation of the Nonesuch results. 16 refs., 14 figs., 2 tabs.
- Research Organization:
- Indiana Univ., Bloomington, IN (USA)
- Sponsoring Organization:
- DOE/ER
- DOE Contract Number:
- FG02-88ER13978
- OSTI ID:
- 5628359
- Report Number(s):
- DOE/ER/13978-1; ON: DE89017561
- Country of Publication:
- United States
- Language:
- English
Similar Records
Organic geochemical and tectonic evolution of the midcontinent rift system: Organic geochemistry and micropaleontology
Organic geochemical and tectonic evolution of the midcontinent rift system: Organic geochemistry and micropaleontology
Sterane and triterpane biomarkers in the Precambrian Nonesuch Formation, North American Midcontinent Rift
Technical Report
·
Fri Jun 01 00:00:00 EDT 1990
·
OSTI ID:6866228
Organic geochemical and tectonic evolution of the midcontinent rift system: Organic geochemistry and micropaleontology
Technical Report
·
Mon Dec 31 23:00:00 EST 1990
·
OSTI ID:5835377
Sterane and triterpane biomarkers in the Precambrian Nonesuch Formation, North American Midcontinent Rift
Journal Article
·
Thu Feb 28 23:00:00 EST 1991
· Geochimica et Cosmochimica Acta; (United States)
·
OSTI ID:5912702
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
CARBONATE ROCKS
CHEMISTRY
DOCUMENT TYPES
FEDERAL REGION V
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGY
LIMESTONE
MICHIGAN
MINERAL RESOURCES
NORTH AMERICA
PETROLEUM DEPOSITS
PROGRESS REPORT
RESOURCES
ROCKS
SEDIMENTARY ROCKS
SHALES
SOURCE ROCKS
STRATIGRAPHY
USA
WISCONSIN
020200* -- Petroleum-- Reserves
Geology
& Exploration
CARBONATE ROCKS
CHEMISTRY
DOCUMENT TYPES
FEDERAL REGION V
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGY
LIMESTONE
MICHIGAN
MINERAL RESOURCES
NORTH AMERICA
PETROLEUM DEPOSITS
PROGRESS REPORT
RESOURCES
ROCKS
SEDIMENTARY ROCKS
SHALES
SOURCE ROCKS
STRATIGRAPHY
USA
WISCONSIN