Geochemistry of regionally extensive dolomites, Burlington and Keokuk Formations (Mississippian), Iowa and Illinois
Conference
·
· Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5961532
The Burlington and Keokuk Formations (Mississippian) contain 2 major generations of dolomite throughout the several ten-thousand square kilometers of study area. Dolomite I (oldest) is luminescently zoned, Ca-rich, Fe- and Mn-poor, and has Mississippian /sup 87/Sr//sup 86/Sr; dolomite II is unzoned, nearly stoichiometric, Fe- and Mn-rich, and has radiogenic /sup 87/Sr//sup 86/Sr; dolomite III, a minor zone, is nonluminescent and very Fe-rich. Dolomites I and II formed before nonmarine calcite cements, and all dolomites formed before Late Mississippian under shallow burial conditions. Stable isotopes of dolomite I average +2.3 per thousand delta/sup 13/C and -0.3 per thousand delta/sup 18/O PDB. Dolomite I is slightly depleted in /sup 13/C and /sup 18/O with respect to estimated Mississippian marine dolomite. Thus, dolomite I may have formed in waters only slightly depleted in /sup 18/O and /sup 13/C compared with seawater at low temperatures (approx. 25/sup 0/C). Dolomite II averages -4.1 per thousand delta/sup 18/O PDB, +2.8 per thousand delta/sup 13/C PDB, and has a wide range of delta/sup 18/O (-0.5 to -6.6 per thousand PDB) and a narrower range of delta/sup 13/C (+1 to +4 per thousand). These data suggest that temperatures of precipitation were less than the 80/sup 0/C-110/sup 0/C ranges implied by the contained 2-phase fluid inclusions, unless the waters were isotopically heavy (approx. +3 to 11 per thousand delta/sup 18/O SMOW). Dolomite II shows a regional geographic trend of decreasing delta/sup 18/O and increasing delta/sup 13/ from north to south. This trend can be accounted for by either a northward decrease in temperature or in /sup 18/O content of diagenetic waters.
- Research Organization:
- State Univ. of New York, Stony Brook
- OSTI ID:
- 5961532
- Report Number(s):
- CONF-850322-
- Conference Information:
- Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 69:2
- Country of Publication:
- United States
- Language:
- English
Similar Records
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Calcite veins of the Stripa granite (Sweden) as records of the origin of the ground waters and their interactions with the granitic body
Petrologic and geochemical constraints on the origin of regionally extensive dolomites of the Mississippian Burlington and Keokuk fms. , Iowa, Illinois and Missouri
Journal Article
·
Tue Oct 01 00:00:00 EDT 1991
· Geochimica et Cosmochimica Acta; (United States)
·
OSTI ID:7302560
Calcite veins of the Stripa granite (Sweden) as records of the origin of the ground waters and their interactions with the granitic body
Journal Article
·
Tue Aug 01 00:00:00 EDT 1989
· Geochimica et Cosmochimica Acta; (USA)
·
OSTI ID:7079404
Petrologic and geochemical constraints on the origin of regionally extensive dolomites of the Mississippian Burlington and Keokuk fms. , Iowa, Illinois and Missouri
Thesis/Dissertation
·
Tue Dec 31 23:00:00 EST 1985
·
OSTI ID:5097352
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
ALKALINE EARTH METAL COMPOUNDS
CALCIUM CARBONATES
CALCIUM COMPOUNDS
CARBON COMPOUNDS
CARBONATE MINERALS
CARBONATES
CHEMISTRY
DIAGENESIS
DOLOMITE
FEDERAL REGION V
FEDERAL REGION VII
GEOCHEMISTRY
GEOLOGIC AGES
GEOLOGIC FORMATIONS
ILLINOIS
IOWA
MAGNESIUM CARBONATES
MAGNESIUM COMPOUNDS
MINERALS
MISSISSIPPIAN PERIOD
NORTH AMERICA
OXYGEN COMPOUNDS
PALEOZOIC ERA
RESERVOIR ROCK
USA
020200* -- Petroleum-- Reserves
Geology
& Exploration
ALKALINE EARTH METAL COMPOUNDS
CALCIUM CARBONATES
CALCIUM COMPOUNDS
CARBON COMPOUNDS
CARBONATE MINERALS
CARBONATES
CHEMISTRY
DIAGENESIS
DOLOMITE
FEDERAL REGION V
FEDERAL REGION VII
GEOCHEMISTRY
GEOLOGIC AGES
GEOLOGIC FORMATIONS
ILLINOIS
IOWA
MAGNESIUM CARBONATES
MAGNESIUM COMPOUNDS
MINERALS
MISSISSIPPIAN PERIOD
NORTH AMERICA
OXYGEN COMPOUNDS
PALEOZOIC ERA
RESERVOIR ROCK
USA