Occurrence and formation of dolomite in organic-rich continental margin sediments

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doi: 10.1306/94885570-1704-11D7-8645000102C1865D
Author(s): Baker, Paul A.; Burns, Stephen J.
Author Affiliation(s): Primary:
Duke Univ., Dep. Geol., Durham, NC, United States
Volume Title: AAPG Bulletin
Source: AAPG Bulletin, 69(11), p.1917-1930. Publisher: American Association of Petroleum Geologists, Tulsa, OK, United States. ISSN: 0149-1423 CODEN: AABUD2
Note: In English. 106 refs.; illus. incl. 2 tables, sketch map
Summary: Dolomite forms in sediments over large areas of the ocean-floor. The most common environment is organic-rich calcareous continental margin sediments.
Year of Publication: 1985
Research Program: DSDP Deep Sea Drilling Project
Key Words: 06 Petrology, Sedimentary; Alkaline earth metals; Bibliography; California; Carbonate rocks; Carbonatization; Cenozoic; Continental margin; Controls; Deep Sea Drilling Project; Diagenesis; Dolomitization; Dolostone; Early diagenesis; Genesis; Geochemistry; Global; Magnesium; Marine sediments; Metals; Miocene; Monterey Formation; Neogene; Organic compounds; Organic materials; Pore water; Rates; Review; Sedimentary petrology; Sedimentary rocks; Sediments; Tertiary; United States
Record ID: 1986030592
Copyright Information: GeoRef, Copyright 2017 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom

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