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Influence of depositional environment on sandstone diagenesis (view source)
Revision as of 20:26, 8 May 2015
, 20:26, 8 May 2015→Diagenesis and depositional pore waters
==Diagenesis and depositional pore waters==
==Diagenesis and depositional pore waters==
In the Wilcox of the Texas Gulf Coast, certain minerals precipitate as a result of the influence of depositional pore-water chemistry:<ref name=ch09r60><ref name=ch09r59>Stonecipher, S., A., May, J., A., 1990, [http://archives.datapages.com/data/specpubs/resmi1/data/a065/a065/0001/0000/0025.htm Facies controls on early diagenesis: Wilcox Group, Texas Gulf Coast], in Meshri, D., Ortoleva, P., J., eds., Prediction of Reservoir Quality Through Chemical Modeling: AAPG Memoir 49, p. 25–44.</ref>
In the Wilcox of the Texas Gulf Coast, certain minerals precipitate as a result of the influence of depositional pore-water chemistry:<ref name=ch09r60 /><ref name=ch09r59>Stonecipher, S., A., May, J., A., 1990, [http://archives.datapages.com/data/specpubs/resmi1/data/a065/a065/0001/0000/0025.htm Facies controls on early diagenesis: Wilcox Group, Texas Gulf Coast], in Meshri, D., Ortoleva, P., J., eds., Prediction of Reservoir Quality Through Chemical Modeling: AAPG Memoir 49, p. 25–44.</ref>
* Mica-derived kaolinite characterizes fluvial/distributary-channel sands flushed by fresh water
* Mica-derived kaolinite characterizes fluvial/distributary-channel sands flushed by fresh water