Mutti, Maria (1998): Early to middle Miocene carbonate chemostratigraphy and compositional changes of shelf-derived turbidites from ODP Leg 165, Site 1000, northern Nicaraguan Rise and Site 999, Colombian Basin

Leg/Site/Hole:
ODP 165
ODP 165 1000
ODP 165 999
Identifier:
1999-010429
georefid

Creator:
Mutti, Maria
University of Southern California, Los Angeles, CA, United States
author

Identification:
Early to middle Miocene carbonate chemostratigraphy and compositional changes of shelf-derived turbidites from ODP Leg 165, Site 1000, northern Nicaraguan Rise and Site 999, Colombian Basin
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
The recovered succession at Site 1000 consists dominantly of peri-platform sediments and sedimentary rocks, interbedded with intervals of redeposited pelagic and neritic carbonate sediments from the slopes and tops of the adjacent shallow water banks. Site 999 is situated offshore from the Nicaraguan Rise, in the pelagic environment of the Colombia Basin, and the recovered succession there is 1066,4 m thick and consists primarily of pelagic rocks.
English
Coverage:Geographic coordinates:
North:22.0000
West:-79.5200East: -60.0000
South:9.0000

Stratigraphy; Isotope geochemistry; Atlantic Ocean; C-13/C-12; carbon; carbonate platforms; Caribbean Sea; Cenozoic; chemostratigraphy; Colombian Basin; composition; isotope ratios; isotopes; Leg 165; lithofacies; lower Miocene; marine environment; middle Miocene; Miocene; Neogene; Nicaragua Rise; North Atlantic; Ocean Drilling Program; ODP Site 1000; ODP Site 999; paleo-oceanography; Pedro Channel; pelagic environment; provenance; shelf environment; stable isotopes; Tertiary; thickness; turbidite;

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