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• W2080212705 abstract "Research Article| April 01, 2012 Climate change and the formation of nickel laterite deposits Robert L. Thorne; Robert L. Thorne 1School of Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK2CSIRO Earth Science and Resource Engineering, Australian Resources and Research Centre, Kensington, Western Australia 6151, Australia Search for other works by this author on: GSW Google Scholar Stephen Roberts; Stephen Roberts 1School of Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar Richard Herrington Richard Herrington 3Department of Mineralogy, Natural History Museum, Cromwell Road, London SW7 5BD, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Robert L. Thorne 1School of Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK2CSIRO Earth Science and Resource Engineering, Australian Resources and Research Centre, Kensington, Western Australia 6151, Australia Stephen Roberts 1School of Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Richard Herrington 3Department of Mineralogy, Natural History Museum, Cromwell Road, London SW7 5BD, UK Publisher: Geological Society of America Received: 13 Jun 2011 Revision Received: 07 Nov 2011 Accepted: 15 Nov 2011 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2012 Geological Society of America Geology (2012) 40 (4): 331–334. https://doi.org/10.1130/G32549.1 Article history Received: 13 Jun 2011 Revision Received: 07 Nov 2011 Accepted: 15 Nov 2011 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Robert L. Thorne, Stephen Roberts, Richard Herrington; Climate change and the formation of nickel laterite deposits. Geology 2012;; 40 (4): 331–334. doi: https://doi.org/10.1130/G32549.1 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 One of the major controls on nickel laterite deposit formation is climate. A comparison of climatic data for regions where ultramafic rocks are exposed shows that areas currently conducive to nickel laterite formation receive >1000 mm/yr precipitation, have cold month mean (CMM) temperatures between 15 and 27 °C, and warm month mean (WMM) temperatures between 22 and 31 °C. Using a compilation of paleoclimatic data and the defined climatic window of nickel laterite deposit formation allows an assessment of the timing and duration of paleo–nickel laterite formation in ancient terrains. To illustrate the potential of this technique, we show that the formation of the Çaldağ nickel laterite deposit of western Turkey most likely initiated when the ultramafic protolith of Cretaceous age was exposed in the Early Eocene, and that the majority of the deposit formed during the Eocene. In contrast, the formation of the Bitincke deposit, south Albania, was mostly complete by the Early Eocene, after which CMM temperatures dropped below the optimum for laterite formation. 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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