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• W2092168959 abstract "Research Article| December 01, 2006 The fate of diamondoids in coals and sedimentary rocks Zhibin Wei; Zhibin Wei 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Search for other works by this author on: GSW Google Scholar J. Michael Moldowan; J. Michael Moldowan 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Search for other works by this author on: GSW Google Scholar Daniel M. Jarvie; Daniel M. Jarvie 2Humble Geochemical Services, Division of Humble Instruments & Services, Inc., P.O. Box 789, Humble, Texas 77347, USA Search for other works by this author on: GSW Google Scholar Ronald Hill Ronald Hill 3U.S. Geological Survey, Box 25046, Denver Federal Center, MS 939, Denver, Colorado 80225, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Zhibin Wei 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA J. Michael Moldowan 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Daniel M. Jarvie 2Humble Geochemical Services, Division of Humble Instruments & Services, Inc., P.O. Box 789, Humble, Texas 77347, USA Ronald Hill 3U.S. Geological Survey, Box 25046, Denver Federal Center, MS 939, Denver, Colorado 80225, USA Publisher: Geological Society of America Received: 23 Mar 2006 Revision Received: 26 Jun 2006 Accepted: 28 Jun 2006 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 The Geological Society of America, Inc. Geology (2006) 34 (12): 1013–1016. https://doi.org/10.1130/G22840A.1 Article history Received: 23 Mar 2006 Revision Received: 26 Jun 2006 Accepted: 28 Jun 2006 First Online: 09 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 Zhibin Wei, J. Michael Moldowan, Daniel M. Jarvie, Ronald Hill; The fate of diamondoids in coals and sedimentary rocks. Geology 2006;; 34 (12): 1013–1016. doi: https://doi.org/10.1130/G22840A.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 SocietyGeology Search Advanced Search Abstract Diamondoids were detected in the extracts of a series of coals and rocks varying in maturity, lithology, source input, and depositional environment. At the same maturity level, diamondoids are generally about a magnitude more abundant in source rocks than in coals. The concentrations of diamondoids are maturity dependent. However, while diamondoids become more abundant with the increasing thermal maturity, a diminution in diamondoid concentrations is observed at the maturity value of about Ro = 4.0% in both coals and rocks. The occurrence of diamantane destruction at 550 °C during pyrolysis suggests that diamondoids may be eventually destroyed at high temperatures in the Earth. Here we propose three main phases of diamondoid life in nature: diamondoid generation (phase I, Ro < 1.1%), diamondoid generation and enrichment (phase II, 1.1% ≤ Ro ≤ 4.0%), and diamondoid destruction (phase III, Ro > 4.0%). 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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• W2092168959 title "The fate of diamondoids in coals and sedimentary rocks" @default.
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