Origin and chemical evolution of formation waters from Silurian-Devonian strata in the Illinois basin, USA
- Southern Illinois Univ., Edwardsville (USA)
- Univ. of Michigan, Ann Arbor (USA)
A suite of formation-water samples from Silurian-Devonian reservoirs in the Illinois basin has been analyzed for major, minor, and trace element concentrations and for H, O, and Sr isotopic compositions in order to interpret origin of salinity and geochemical evolution of brine compositions in this evaporite- and shale-poor cratonic basin. Although chloride concentrations range from 2,000 to 137,000 mg/L, Cl/Br ratios (291 {plus minus} 18) are consistent with those of seawater or seawater evaporated short of halite saturation (Cl/Br = 292). Thus, during Silurian-Devonian time, subaerially evaporated, penesaline brine entered the subsurface where it was chemically modified through brine-rock interactions. Cation/Br ratios and mineralogy of associated strata indicate that Na and K were depleted through interaction with clay minerals, Ca was enriched and Mg depleted by dolomitization, and Sr was enriched as a result of CaCO{sub 3} recrystallization and dolomitization. Brine {sup 87}Sr/{sup 86}Sr ratios range from 0.7092 to 0.7108; when these ratios are plotted versus 1/Sr, a two-component mixing trend is suggested, although Sr concentrations have experienced local diagenetic modification. A {sup 87}Sr-enriched fluid may have accompanied petroleum migration from New Albany shales into adjacent Silurian-Devonian carbonates where it mixed with remnant evaporated seawater. This event probably preceded the influx of meteoric water, as {delta}D and {delta}{sup 18}O are not correlated with Sr isotopic compositions of formation waters.
- OSTI ID:
- 5920692
- Journal Information:
- Geochimica et Cosmochimica Acta; (USA), Vol. 55:1; ISSN 0016-7037
- Country of Publication:
- United States
- Language:
- English
Similar Records
Chemistry of fluid inclusions in halite from the Salina group of the Michigan basin: Implications for Late Silurian seawater and the origin of sedimentary brines
Ordovician carbonate formation waters in the Illinois Basin: Chemical and isotopic evolution beneath a regional aquitard
Related Subjects
BRINES
CHEMICAL COMPOSITION
GEOCHEMISTRY
ROCK-FLUID INTERACTIONS
ILLINOIS BASIN
DEVONIAN PERIOD
GEOLOGIC STRATA
ISOTOPE RATIO
MINERALIZATION
SEAWATER
SILURIAN PERIOD
STRONTIUM 87
ALKALINE EARTH ISOTOPES
BETA DECAY RADIOISOTOPES
CHEMISTRY
ELECTRON CAPTURE RADIOISOTOPES
EVEN-ODD NUCLEI
GEOLOGIC AGES
GEOLOGIC STRUCTURES
HOURS LIVING RADIOISOTOPES
HYDROGEN COMPOUNDS
INTERMEDIATE MASS NUCLEI
ISOMERIC TRANSITION ISOTOPES
ISOTOPES
NUCLEI
OXYGEN COMPOUNDS
PALEOZOIC ERA
RADIOISOTOPES
STABLE ISOTOPES
STRONTIUM ISOTOPES
WATER
580000* - Geosciences