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Title: Lithologic controls on morphology of pressure-dissolution surfaces (stylolites and dissolution seams) in Paleozoic carbonate rocks from the mideastern United States

Journal Article · · Journal of Sedimentary Petrology; (United States)
DOI:https://doi.org/10.2110/jsr.63.513· OSTI ID:6383835
 [1]
  1. Univ. of Georgia, Athens (United States)

Examination of pressure-dissolution surfaces (stylolites and dissolution seams) in carbonate rocks from the mideastern US demonstrates that the morphology of these surfaces varies with rock fabric. In limestones, pressure dissolution causes suturing of intergranular contacts at the microscopic scale and formation of macroscopic pressure-dissolution surfaces. Pressure dissolution thus modifies limestone fabric, and it contributes to destruction of porosity in two ways, by eliminating intergranular space at sites of dissolution and by providing cement to fill pores elsewhere. In addition to these petrologic effects, pressure-dissolution surfaces (1) can generate bedding planes, (2) can account for significant thicknesses of lost section in stratigraphic reconstructions, and (3) can be of economic significance by modifying reservoir properties, by serving as barriers to petroleum migration, and by acting as seals for reservoirs. This paper examines lithologic controls on morphology of stylolites and dissolution seams in relatively undeformed carbonate rocks. It thus addresses many of the same problems on which Buxton and Sibley (1981) focused, but it quantifies, rather than categorizes, morphology of pressure-dissolution surfaces, and examines a more general sample suite from the mideastern US.

OSTI ID:
6383835
Journal Information:
Journal of Sedimentary Petrology; (United States), Vol. 63:3; ISSN 0022-4472
Country of Publication:
United States
Language:
English