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- W2078194465 endingPage "B31169.1" @default.
- W2078194465 startingPage "B31169.1" @default.
- W2078194465 abstract "Research Article| July 01, 2015 Clumped isotope thermometry in deeply buried sedimentary carbonates: The effects of bond reordering and recrystallization Brock J. Shenton; Brock J. Shenton † 1Texas A&M University (TAMU), Department of Geology & Geophysics, College Station, Texas 77843, USA †brock.shenton@gmail.com. Search for other works by this author on: GSW Google Scholar Ethan L. Grossman; Ethan L. Grossman 1Texas A&M University (TAMU), Department of Geology & Geophysics, College Station, Texas 77843, USA Search for other works by this author on: GSW Google Scholar Benjamin H. Passey; Benjamin H. Passey 2Johns Hopkins University, Department of Earth & Planetary Sciences, Baltimore, Maryland 21218, USA Search for other works by this author on: GSW Google Scholar Gregory A. Henkes; Gregory A. Henkes 2Johns Hopkins University, Department of Earth & Planetary Sciences, Baltimore, Maryland 21218, USA Search for other works by this author on: GSW Google Scholar Thomas P. Becker; Thomas P. Becker 3ExxonMobil Upstream Research Company, P.O. Box 2189, Houston, Texas 77252-2189, USA Search for other works by this author on: GSW Google Scholar Juan Carlos Laya; Juan Carlos Laya 1Texas A&M University (TAMU), Department of Geology & Geophysics, College Station, Texas 77843, USA Search for other works by this author on: GSW Google Scholar Alberto Perez-Huerta; Alberto Perez-Huerta 4University of Alabama, Department of Geological Sciences, Tuscaloosa, Alabama 35487, USA Search for other works by this author on: GSW Google Scholar Stephen P. Becker; Stephen P. Becker 3ExxonMobil Upstream Research Company, P.O. Box 2189, Houston, Texas 77252-2189, USA Search for other works by this author on: GSW Google Scholar Michael Lawson Michael Lawson 3ExxonMobil Upstream Research Company, P.O. Box 2189, Houston, Texas 77252-2189, USA Search for other works by this author on: GSW Google Scholar GSA Bulletin (2015) 127 (7-8): 1036–1051. https://doi.org/10.1130/B31169.1 Article history received: 17 Jul 2014 rev-recd: 05 Nov 2014 accepted: 14 Jan 2015 first online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Brock J. Shenton, Ethan L. Grossman, Benjamin H. Passey, Gregory A. Henkes, Thomas P. Becker, Juan Carlos Laya, Alberto Perez-Huerta, Stephen P. Becker, Michael Lawson; Clumped isotope thermometry in deeply buried sedimentary carbonates: The effects of bond reordering and recrystallization. GSA Bulletin 2015;; 127 (7-8): 1036–1051. doi: https://doi.org/10.1130/B31169.1 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 SocietyGSA Bulletin Search Advanced Search Abstract We utilize carbonate clumped isotope thermometry to explore the diagenetic and thermal histories of exhumed brachiopods, crinoids, cements, and host rock in the Permian Palmarito Formation, Venezuela, and the Carboniferous Bird Spring Formation, Nevada, USA. Carbonate components in the Palmarito Formation, buried to ∼4 km depth, yield statistically indistinguishable clumped isotope temperatures [T(Δ47)] ranging from 86 to 122 °C. Clumped isotope temperatures of components in the more deeply buried Bird Spring Formation (>5 km) range from ∼100 to 165 °C and differ by component type, with brachiopods and pore-filling cements yielding the highest T(Δ47) (mean = 153 and 141 °C, respectively) and crinoids and host rock yielding significantly cooler T(Δ47) (mean = 103 and 114 °C). New high-resolution thermal histories are coupled with kinetic models to predict the extent of solid-state C-O bond reordering during burial and exhumation for both sites. Application of these models, termed “THRMs” (thermal history reordering models), suggests that brachiopods in the Palmarito Formation experienced partial bond reordering without complete equilibration of clumped isotopes at maximum burial temperature. In contrast, clumped isotope bonds of brachiopods from the Bird Spring Formation completely equilibrated at maximum burial temperature, and now reflect blocking temperatures achieved during cooling. The 40–50-°C-cooler clumped isotope temperatures measured in Bird Spring Formation crinoids and host rock can be explained by recrystallization and cementation during shallow burial combined with a greater inherent resistance to solid-state reordering than brachiopods. 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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- W2078194465 date "2015-02-19" @default.
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- W2078194465 title "Clumped isotope thermometry in deeply buried sedimentary carbonates: The effects of bond reordering and recrystallization" @default.
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