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Volume 29 Issue 3
Aug 2018
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Journal of Earth Science  > 2018  >  29(3): 520-536.
Yu Shi, Yuwang Wang, Jingbin Wang, Lutong Zhao, Hongjing Xie, Lingli Long, Tao Zou, Dedong Li, Guochao Zhou. Physicochemical Control of the Early Permian Xiangshan Fe-Ti Oxide Deposit in Eastern Tianshan (Xinjiang), NW China. Journal of Earth Science, 2018, 29(3): 520-536. doi: 10.1007/s12583-017-0969-4
Citation: Yu Shi, Yuwang Wang, Jingbin Wang, Lutong Zhao, Hongjing Xie, Lingli Long, Tao Zou, Dedong Li, Guochao Zhou. Physicochemical Control of the Early Permian Xiangshan Fe-Ti Oxide Deposit in Eastern Tianshan (Xinjiang), NW China. Journal of Earth Science, 2018, 29(3): 520-536. doi: 10.1007/s12583-017-0969-4
shu

Physicochemical Control of the Early Permian Xiangshan Fe-Ti Oxide Deposit in Eastern Tianshan (Xinjiang), NW China

doi: 10.1007/s12583-017-0969-4
  • 1.

    Beijing Institute of Geology for Mineral Resources, Beijing 100012, China

  • 2.

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

  • 3.

    Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China

More Information
  • Corresponding author: Yu Shi, orounaxiong@sina.com
  • Received Date: 17 Jan 2017
  • Accepted Date: 10 May 2017
  • Publish Date: 01 Jun 2018
    Abstract
  • The Xiangshan mafic-ultramafic complex is one of the major Early Permian mafic- ultramafic intrusions in eastern Tianshan (Xinjiang, NW China), and consists of two major intrusive phases. The first intrusive phase is mainly gabbroic rocks hosting ilmenite mineralization, while the second intrusive phase is mainly lherzoilite associated with Ni-Cu sulfide mineralization. The Xiangshan ilmenite orebodies hosted in the Fe-Ti oxide-bearing gabbro occur along the contact between hornblende gabbros and leucogabbros. The hornblende gabbros and Fe-Ti oxide rich gabbros at Xiangshan are newly dated to be Early Permian (280.1 and 279.2 Ma, respectively). Major and trace element compositions of zircons and whole rocks from Xiangshan hornblende gabbro and Fe-Ti oxide gabbro have been measured by in situ excimer laser ablation ICP-MS. Zircon Ce4+/Ce3+ ratios based on lattice-strain model and Ti-in-zircon temperatures of hornblende gabbro and Fe-Ti oxide gabbro of the Xiangshan complex are calculated to evaluate the physicochemical variations during the ilmenite mineralization. Whole-rock geochemistry and zircon trace element geochemistry suggest that Fe-Ti oxide gabbros were formed from a basaltic parent magma which had undergone a transfromation from being H2O-rich to H2O-poor. During the magmatic evolution, primitive, H2O-poor basaltic melts may have been replenished into the system, increasing its solidus temperature and decreasing its oxygen fugacity and H2O contents. This may have supperessed the Ti-rich poikilitic hornblende fractionation and promoted the plagioclase fractionation, which consequently concentrated the ore-forming components in the residual melts and generated the ilmenite mineralization

     

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