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Petrography stable-isotope geochemistry and diagenesis of Miocene sandstones, Vermilion Block 31, offshore Louisiana

Conference · · AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
OSTI ID:6180744

Sandstones from three conventional cores between depths of 11,140 and 14,910 ft (3345 and 4545 m) currently have an average composition of Q/sub 86/F/sub 10/R/sub 4/, but have lost approximately 5% feldspar to replacement by carbonates and to dissolution. Like other deeply buried Gulf Coast sandstones, plagioclase is being albitized and K-feldspar is dissolving. Patterns of feldspar distribution in the deeper cores suggest that tight cementation by calcite retarded feldspar diagenesis and that waters of different composition or temperature must have invaded different sandstone beds in close proximity. Calcite, quartz, and chlorite are most responsible for causing deterioration of reservoir quality. Calcite volume averages 4.8% and occludes all pores in samples containing more than 5% calcite. Textural relations and isotopic data indicate that calcite precipitated over a broad temperature range and from fluids of variable composition during burial. The /sup 87/Sr//sup 86/Sr ratio of cements is consistent with the derivation of the Sr from coeval, or only very slightly older skeletal material, prior to extensive silicate reactions.

Research Organization:
Univ. of Texas, Austin (USA)
OSTI ID:
6180744
Report Number(s):
CONF-8810362-
Journal Information:
AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States), Journal Name: AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) Vol. 72:9; ISSN AABUD
Country of Publication:
United States
Language:
English