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Chen Yanhong, Yang Jingsui, 2018. Formation of Podiform Chromitite Deposits: Review and Prospects. Earth Science, 43(4): 991-1010. doi: 10.3799/dqkx.2018.704
Citation: Chen Yanhong, Yang Jingsui, 2018. Formation of Podiform Chromitite Deposits: Review and Prospects. Earth Science, 43(4): 991-1010. doi: 10.3799/dqkx.2018.704
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Formation of Podiform Chromitite Deposits: Review and Prospects

doi: 10.3799/dqkx.2018.704
  • 1.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

  • 2.

    Center for Advanced Research on Mantle(CARMA), Key Laboratory of Deep-Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

  • Received Date: 2017-12-18
  • Publish Date: 2018-04-15
    Abstract
  • As the characteristic ore deposits in ophiolites, podiform chromitite deposits mainly formed in the ultramafic section of an ophiolite complex. However, the following issues on podiform chromitite remain controversial:(1) crystal-melt separation; (2) residual of mantle partial melting; (3) melt-rock interaction. It is of particular importance to study the formation processes of podiform chromitite when large amounts of unusual minerals are found in podiform chromitite and its host rock peridotite. Petrogeneses of chromitite are reviewed in this paper. The pMELTS thermodynamic software was used to calculate the contribution of shallow mantle processes to the formation of podiform chromitite. Preliminary simulation results show that it is impossible to explain the formation of large-scale podiform chromitite deposits by individual mantle partial melting, mantle melt separation or tholeiitic melt-depleted mantle interaction processes, which implies that the podiform chromitite deposits may have been formed by multi-stage or deep mantle processes. Further researches are needed to be conducted on the origin of podiform chromitite deposits.

     

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