Dolomitization in Smackover Formation, Escambia County, Alabama
Dolomitization is critical to the development of reservoir porosity in the Smackover Formation of southeastern Alabama, as seen in the Appleton and Big Escambia Creek fields. Dolomitization is concentrated in permeable facies on depositional highs. In both fields, the dolomitizing fluids were geochemically similar to the waters in which deposition occurred. Deposition and dolomitization near Appleton field (near the updip limit of the Smackover Formation) occurred in more saline waters than basinward in the Big Escambia Creek field. The Smackover Formation in the Appleton field was deposited in supratidal, intertidal, and shallow lagoonal environments. Abundant bluegreen algal structures and the absence of normal marine fossils indicate the lagoonal waters were hypersaline. In the western part of Big Escambia Creek field, dolomitization is concentrated in the upper Smackover Formation in ooid-peloid grainstones that accumulated on a syndepositional high. Bioturbated peloid packstones and wackestones accumulated in deeper water off the syndepositional high and are not pervasively dolomitized. Rhodolites and calcareous fossil fragments indicate deposition in or near seawater with normal marine salinities.
- Research Organization:
- Cities Service Oil and Gas Corp., Tulsa, OK
- OSTI ID:
- 6931820
- Report Number(s):
- CONF-8610199-
- Journal Information:
- Am. Assoc. Pet. Geol., Bull.; (United States), Vol. 70:9; Conference: 36. annual meeting of the Gulf Coast Association Geological Societies and the Gulf Coast Section of SEPM, Baton Rouge, LA, USA, 22 Oct 1986
- Country of Publication:
- United States
- Language:
- English
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Depositional history of the Smackover Formation, Appleton Field, Escambia County, Alabama
Depositional history of the Smackover Formation, Appleton Field, Escambia County, Alabama
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