High-salinity overpressured fluids associated with MVT mineralization Shady Dolomite (Cambrian), Virginia
In Virginia, MVT Pb-Zn deposits are present in platform margin carbonates of the Lower Cambrian Shady Dolomite. Ore deposition occurred during late Paleozoic thrust faulting and was preceded by dissolution and brecciation of host carbonates, creating a porous and permeable network for later mineralizing fluids. Ore mineralization was followed by precipitation of saddle dolomite, authigenic quartz, and calcite. Large pseudosecondary fluid inclusions (up to 30-40 m) in authigenic quartz contain a liquid and vapor phase and halite daughter minerals. The L-V (L) occurred between 110 and 140C; total homogenization (by halite disappearance) occurred at 176-225C. Salinities, based on TM (halite), are estimated to be 31-33 wt. % NaCl equivalent, assuming a pure NaCl-H/sub 2/O system. However, Te (-26 to -25C) indicates the presence of divalent cations (Ca/sup 2//sup +/ and/or Mg/sup 2//sup +/). Minimum trapping pressures, estimated from the intersections of the inclusion isochores with the liquidus curves corresponding to inclusion salinities, range from 430 to 1,370 bars. The range of pressures and temperatures thus obtained exceeds that defined by hydrostatic load (100 bars/km), using the likely range of geothermal gradients (20-35C/km). The fluids forming the inclusions, therefore, were overpressured, which is consistent with other evidence indicating the former presence of overpressured fluids. A minimum depth of formation calculated from the lowest temperature of total homogenization (176C) using a geothermal gradient of 35C/km is about 4-5 km, consistent with the estimated 5-km thick overlying Paleozoic section. Maximum burial depth estimated by projecting the isochores delimiting the P-T conditions of fluid inclusion formation up to a maximum temperature of 250C is about 6-7 km. This additional pressure could be generated by tectonic thickening during thrusting.
- OSTI ID:
- 6544401
- Report Number(s):
- CONF-880301-
- Resource Relation:
- Conference: Annual meeting of the American Association of Petroleum Geologists, Houston, TX, USA, 20 Mar 1988
- Country of Publication:
- United States
- Language:
- English
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03 NATURAL GAS
NATURAL GAS DEPOSITS
GEOCHEMISTRY
PETROLEUM DEPOSITS
RESERVOIR FLUIDS
SALINITY
VIRGINIA
BRINES
CALCITE
CAMBRIAN PERIOD
CARBONATE ROCKS
DOLOMITE
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GEOLOGIC FAULTS
LEAD
MINERALIZATION
QUARTZ
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ALKALINE EARTH METAL COMPOUNDS
CALCIUM CARBONATES
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CARBON COMPOUNDS
CARBONATE MINERALS
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FEDERAL REGION III
FLUIDS
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
MAGNESIUM CARBONATES
MAGNESIUM COMPOUNDS
METALS
MINERAL RESOURCES
MINERALS
NORTH AMERICA
OXIDE MINERALS
OXIDES
OXYGEN COMPOUNDS
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SEDIMENTARY ROCKS
SILICON COMPOUNDS
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USA
020200* - Petroleum- Reserves
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& Exploration
030200 - Natural Gas- Reserves
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