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Organic geochemical and tectonic evolution of the midcontinent rift system: Organic geochemistry and micropaleontology

Technical Report ·
DOI:https://doi.org/10.2172/6866228· OSTI ID:6866228
;  [1];  [2]
  1. Indiana Univ., Bloomington, IN (USA). Dept. of Chemistry Indiana Univ., Bloomington, IN (USA). Dept. of Geological Sciences
  2. Harvard Univ., Cambridge, MA (USA). Dept. of Earth and Planetary Sciences
During the second year of funding for this project, we completed routine organic geochemical analyses on a set of about 150 samples of the Nonesuch Formation from cores and outcrops in Wisconsin and Michigan. Hieshima and Lichtfouse traveled to the Iowa Geological Survey in December, 1989 to sample cores and cutting from the M.G. Eischied {number sign}1 Well. This exploration well penetrated over 4,000 meters of Precambrian volcanic and sedimentary strata, ultimately encountering about 400 meters of black shale similar to the Nonesuch at a depth close to 5,000 meters. In February and March of 1990, Hieshima traveled to Australia and worked for two months with Roger Summons (Bureau of Mineral Resources) on the molecular structure of chemical fossils (biomarkers) in the Nonesuch. Isomeric ratios and absolute abundances of both common and novel biomarkers were determined for the saturated and aromatic hydrocarbon fractions of about twenty samples. During May Jeff Mauk (Ph.D. student with William Kelly at the University of Michigan) came to Indiana with carefully collected samples of rocks and petroleums from the White Pine Mine. Analytical data on these samples will provide a basis for comparison of thermal maturity and chemical alteration between the Nonesuch within and outside the zone of copper mineralization.
Research Organization:
Indiana Univ. Foundation, Bloomington, IN (USA)
Sponsoring Organization:
DOE/ER
DOE Contract Number:
FG02-88ER13978
OSTI ID:
6866228
Report Number(s):
DOE/ER/13978-2; ON: DE90013107
Country of Publication:
United States
Language:
English