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The AAPG/Datapages Combined Publications Database

Journal of Sedimentary Research (SEPM)

Abstract


Journal of Sedimentary Petrology
Vol. 29 (1959)No. 2. (June), Pages 260-266

Diagenesis of Late Cambrian Oolitic Limestone, Previous HitMauriceNext Hit Formation, Montana and Wyoming

C. W. Brown

ABSTRACT

Dolomitization of Late Cambrian oolitic limestone in the Previous HitMauriceNext Hit Formation followed lithification and preceded regional fracturing of the rock. The source of Mg-rich dolomitizing solutions is believed to have been connate waters from adjacent argillaceous sediments. Regional compaction forced these waters into the permeable oolite sands of the Previous HitMauriceTop Formation. Fluid migration and subsequent dolomitization were controlled by effective porosity trends essentially parallel to bedding. Aragonitic oolite nuclei formed natural foci for dolomitization.


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