From Organic Matter to Graphite: Graphitization
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Research Article| December 01, 2014 From Organic Matter to Graphite: Graphitization Peter R. Buseck; Peter R. Buseck 1School of Earth and Space Exploration & Department of Chemistry and Biochemistry, Arizona State University, Tempe, AZ 85282, USAE-mail: pbuseck@asu.edu Search for other works by this author on: GSW Google Scholar Olivier Beyssac Olivier Beyssac 2Institut de Minéralogie, de Physique des Matériaux, et de Cosmochimie (IMPMC), Sorbonne Universités - UPMC Université, Paris 06, UMR CNRS 7590 & Muséum National d'Histoire, Naturelle, IRD UMR 206, 4 Place Jussieu, F-75005 Paris, France Search for other works by this author on: GSW Google Scholar Author and Article Information Peter R. Buseck 1School of Earth and Space Exploration & Department of Chemistry and Biochemistry, Arizona State University, Tempe, AZ 85282, USAE-mail: pbuseck@asu.edu Olivier Beyssac 2Institut de Minéralogie, de Physique des Matériaux, et de Cosmochimie (IMPMC), Sorbonne Universités - UPMC Université, Paris 06, UMR CNRS 7590 & Muséum National d'Histoire, Naturelle, IRD UMR 206, 4 Place Jussieu, F-75005 Paris, France Publisher: Mineralogical Society of America First Online: 09 Mar 2017 Online ISSN: 1811-5217 Print ISSN: 1811-5209 © 2014 by the Mineralogical Society of America Elements (2014) 10 (6): 421–426. https://doi.org/10.2113/gselements.10.6.421 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Peter R. Buseck, Olivier Beyssac; From Organic Matter to Graphite: Graphitization. Elements 2014;; 10 (6): 421–426. doi: https://doi.org/10.2113/gselements.10.6.421 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 SocietyElements Search Advanced Search Abstract Organic compounds, which on Earth originate mainly through biological activity, are transformed under the physical conditions of Earth's crust, with the end product being graphite. In this graphitization process, they pass progressively and irreversibly through a wide variety of intermediate macrostructures and nanostructures before finally attaining the stable graphite structure. Characterizing this rich array of carbon structures, which are also of industrial interest, provides valuable information on the geological processes affecting carbon-bearing rocks. These processes impact global energy supplies, the geophysical behavior of the crust, and the habitability of the surface environment. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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