Melim, Leslie A. and Swart, Peter K. (1998): Recognizing marine-burial diagenesis; criteria and examples from Quaternary to Neogene platform to slope carbonates, Bahamas and Florida

Leg/Site/Hole:
ODP 166
ODP 166 1003
ODP 166 1005
Identifier:
1999-010401
georefid

Creator:
Melim, Leslie A.
Western Illinois University, Macomb, IL, United States
author

Swart, Peter K.
University of Miami, United States
author

Identification:
Recognizing marine-burial diagenesis; criteria and examples from Quaternary to Neogene platform to slope carbonates, Bahamas and Florida
1998
In: Anonymous, American Association of Petroleum Geologists 1998 annual meeting
American Association of Petroleum Geologists and Society of Economic Paleontologists and Mineralogists, Tulsa, OK, United States
1998
Marine-burial diagenesis of Neogene platform to slope carbonates takes place in marine pore fluids during shallow burial and results in a mature limestone with moldic porosity, blocky to dogtooth calcite spar, and neomorphism. These fabrics are essentially identical to fabrics long considered diagnostic of meteoric diagenesis but the stable carbon and oxygen isotopic values indicate alteration is seawater. We present three examples from cores in the Bahamas and Florida that document the range of fabrics formed during marine-burial diagenesis in high and low permeability sediments.
English
Coverage:Geographic coordinates:
North:31.0000
West:-87.3000East: -72.0000
South:20.4500

Sedimentary petrology; Bahamas; burial diagenesis; C-13/C-12; calibration; carbon; carbonate platforms; carbonate rocks; carbonates; Caribbean region; Cenozoic; cores; diagenesis; drilling; fabric; Florida; isotope ratios; isotopes; Leg 166; limestone; lithofacies; magnesian calcite; marine environment; meteoric water; mineral composition; Neogene; O-18/O-16; Ocean Drilling Program; ODP Site 1003; ODP Site 1005; oxygen; petrography; pore water; porosity; Quaternary; sea water; sedimentary rocks; slope environment; stable isotopes; Tertiary; United States; West Indies;

.