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Carbonate diagenetic textures from nearsurface diagenetic environments

Journal Article · · Am. Assoc. Pet. Geol. Bull.; (United States)
OSTI ID:7048842

Understanding the processes and products of carbonate diagenesis is essential to exploration for, and optimum development of, hydrocarbon reservoirs in carbonate rocks. Much cementation and formation of secondary porosity in carbonates occurs at relatively shallow depths in one of four major diagenetic environments: the vadose zone, meteoric phreatic zone, mixing zone, and marine phreatic zone. Most carbonates are deposited in and begin their diagenetic history in the marine phreatic environment. With subaerial exposure, fresh water will replace sea water in the pores of shallow-water carbonates, and a zone of mixed fresh and marine waters may form. Diagenesis in the freshwater phreatic environment may involve leaching in the zone of solution, neomorphism of grains accompanied by extensive intergranular calcite cementation in the active saturated zone, or neomorphism of grains without cementation in the stagnant saturated zone.

Research Organization:
Cities Service Research Lab., Tulsa, OK
OSTI ID:
7048842
Journal Information:
Am. Assoc. Pet. Geol. Bull.; (United States), Journal Name: Am. Assoc. Pet. Geol. Bull.; (United States) Vol. 64:4; ISSN AAPGB
Country of Publication:
United States
Language:
English