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    Chromite in the mantle section of the Oman Ophiolite: Implications for the tectonic evolution of the Oman Ophiolite

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    Authors
    Rollinson, Hugh cc
    Adetunji, Jacob cc
    Affiliation
    University of Derby
    Issue Date
    2015-12
    
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    Abstract
    Chromite in the Oman ophiolite is located in the mantle section of the ophiolite sequence and forms abundant small podiformdeposits throughout the length of the ophiolite (Rollinson, 2005).The Oman ophiolite has an exposed mantle section of ca 10 000 km2, and contains ca 200 chromitite bodies. Most are less than 10 000 tonnes and a only a few are >30 000 tonnes (Boudier and Al-Rajhi, 2014). We have examined these deposits in eight different areas of the ophiolite (Figure 1, Rollinson and Adetunji, 2013a), two of which we have studied in great detail – in WadiRajmi in the north of Oman (Rollinson, 2008) and atMaqsad in the south(Rollinson and Adetunji, 2013b).
    Citation
    Rollinson, Hugh and Adetunji, Jacob (2015). Chromite in the Mantle Section of the Oman Ophiolite: Implications for the Tectonic Evolution of the Oman Ophiolite. Acta Geologica Sinica (English Edition), 89(supp. 2): 73-76.
    Publisher
    Wiley
    Journal
    Acta Geologica Sineca
    URI
    http://hdl.handle.net/10545/621505
    DOI
    10.1111/1755-6724.12308_44
    Additional Links
    http://www.geojournals.cn/dzxben/ch/index.aspx
    http://onlinelibrary.wiley.com/wol1/doi/10.1111/1755-6724.12308_44/abstract
    Type
    Article
    Language
    en
    ISSN
    17556724
    ae974a485f413a2113503eed53cd6c53
    10.1111/1755-6724.12308_44
    Scopus Count
    Collections
    Environmental Sustainability Research Centre

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