Immobile Element Fingerprinting of Ophiolites
13. Climate action
14. Life underwater
01 natural sciences
0105 earth and related environmental sciences
DOI:
10.2113/gselements.10.2.101
Publication Date:
2014-04-29T14:41:10Z
AUTHORS (1)
ABSTRACT
Research Article| April 01, 2014 Immobile Element Fingerprinting of Ophiolites Julian A. Pearce *School Earth and Ocean Sciences, Cardiff University, CF10 3AT, UKE-mail: PearceJA@cardiff.ac.uk Search for other works by this author on: GSW Google Scholar Author Article Information Publisher: Mineralogical Society America First Online: 09 Mar 2017 Online ISSN: 1811-5217 Print 1811-5209 © the Elements (2014) 10 (2): 101–108. https://doi.org/10.2113/gselements.10.2.101 history Cite View This Citation Add to Manager Share Icon Facebook Twitter LinkedIn Email Permissions Site Pearce; Ophiolites. 2014;; doi: Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Dropdown Menu input auto suggest filter your All ContentBy SocietyElements Advanced Abstract Much our understanding ocean ridges has come from collection analysis glasses recovered ridge axes. However, applying resulting methodologies ophiolite complexes is not straightforward because ophiolites typically experience intense alteration during their passage subduction zone mountain belt. Instead, immobile element proxies fractionation indices, alkalinity, mantle temperature, flow addition may be used classify lavas fingerprint precise setting at which an formed. The results can help us recognise interpret past spreading centres so make plate tectonic reconstructions. You do have access content, please speak institutional administrator if you feel should access.
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