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Fluid-inclusion temperatures of calcite, formed toward end of paragenetic sequence, fall in the range 74-46 degrees C, uncorrected for pressure. The temperature declined during the successive stages of calcite deposition.
This record provided courtesy of AGI/GeoRef.
This article has been cited by other articles:
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Regional Fluid Flow as a Factor in the Thermal History of the Illinois Basin: Constraints from Fluid Inclusions and the Maturity of Pennsylvanian Coals AAPG Bulletin, February 1, 2002; 86(2): 257 - 277. |
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