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- W2029497310 abstract "Research Article| August 01, 1988 Rapid burial diagenesis of deep-water carbonates: Exuma Sound, Bahamas George R. Dix; George R. Dix 1Heroy Geology Laboratory, Syracuse University, Syracuse, New York 13244-1070 Search for other works by this author on: GSW Google Scholar Henry T. Mullins Henry T. Mullins 1Heroy Geology Laboratory, Syracuse University, Syracuse, New York 13244-1070 Search for other works by this author on: GSW Google Scholar Author and Article Information George R. Dix 1Heroy Geology Laboratory, Syracuse University, Syracuse, New York 13244-1070 Henry T. Mullins 1Heroy Geology Laboratory, Syracuse University, Syracuse, New York 13244-1070 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1988) 16 (8): 680–683. https://doi.org/10.1130/0091-7613(1988)016<0680:RBDODW>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation George R. Dix, Henry T. Mullins; Rapid burial diagenesis of deep-water carbonates: Exuma Sound, Bahamas. Geology 1988;; 16 (8): 680–683. doi: https://doi.org/10.1130/0091-7613(1988)016<0680:RBDODW>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Well-lithified, deep-water, periplatform limestones of late Miocene age occur at subsurface depths from 113 m to total depth of 283 m at Ocean Drilling Program (ODP) Site 632 in Exuma Sound, Bahamas. This occurrence, marked by a dramatic increase in compressional wave velocities up to 5.0 km/s, represents the most rapid transformation of ooze to limestone yet discovered in either periplatform or open-ocean settings. The burial diagenetic pathway is similar to those for meteoric and deep-burial diagenetic environments: aragonite dissolves, magnesian calcites exsolve or dissolve, low-Mg calcite precipitates as cement, and secondary moldic/vuggy porosity develops. Stable isotope ratios suggest precipitation of low-Mg calcite from cold, marine-derived pore waters. Accelerated diagenesis is a response to the influx of large quantities (up to 80%) of bank-derived, metastable carbonates and rapid burial via high accumulation rates (up to 210 m/m.y.). Our findings (1) document carbonate mineral stabilization and lithification in a seawater-mediated, shallow-burial diagenetic environment; (2) highlight the very high diagenetic potential of periplatform carbonates; and (3) call into question the use of seismic velocities as support for the Bahama megabank hypothesis. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W2029497310 title "Rapid burial diagenesis of deep-water carbonates: Exuma Sound, Bahamas" @default.
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