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The association of calcite veins with stylolites in the Smackover Formation of north Louisiana

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:5682174
;  [1]
  1. Texas A and M Univ., College Station (United States)
Small calcite veins in the grainstones of the Upper Smackover Formation of north Louisiana provide insight into the role of stylolites in the late stages of diagenesis of these carbonate rocks. The veins always occur in groups, ranging from a few to swarms. In the two cores examined, vein widths varied from 5 {mu}m to 1 mm and lengths varied from 100 {mu}m to several millimeters. Most veins have one end that terminates at a stylolite; some have both ends terminated by stylolites. The same vein never appears on both sides of a large stylolite, although some veins do cut smaller stylolites. Sets of parallel veins occur at angles to each other in the same swarm - one set cutting the other. The original mineralogy of the veins is calcite. It appears lenticular in thin-section with the long axis of the grains perpendicular to the vein length. Preliminary electron microprobe analyses show the calcite to be relatively pure, containing less than 1% by weight MgCO{sub 3}. However, the calcite does contain slightly more iron than the surrounding micritic matrix. Anhydrite and dolomite frequently replace the calcite in the vein. This replacement generally occurs at the terminus of a vein in a stylolite. Dissolution of the calcite in the veins to produce fracture porosity is also common. The veins are remnants of localized episodic fluid pressure increases that occurred during the latter stages of diagenesis of the Smackover. The same process that formed the veins may have opened the stylolites to fluids that caused the replacement of the veins as well as the later creation of secondary porosity.
OSTI ID:
5682174
Report Number(s):
CONF-910403--
Conference Information:
Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Journal Volume: 75:3
Country of Publication:
United States
Language:
English