Search Results - "Yi, Jiankang"

  • Showing 1 - 4 results of 4
Refine Results
  1. 1

    Anorthosites produced by water-fluxed anatexis of deep arc gabbros, Gangdese batholith, Tibet by Dong, Pengsheng, Weinberg, Roberto F., Zhu, Di-Cheng, Green, Eleanor C.R., Yi, Jiankang, Cawood, Peter A., Li, Shi-Min, Chen, Shaorong

    Published in Earth and planetary science letters (15-12-2024)
    “…•Na- and Sr-rich aqueous fluids caused anatexis of arc gabbros to produce anorthositic melts and garnet + amphibole + epidote residue in the lower…”
    Get full text
    Journal Article
  2. 2

    Early Cretaceous intrusive rocks in the Gangdese arc of southern Tibet do not support shallow subduction of the Neo-Tethyan oceanic lithosphere by Wang, Feng, Wang, Qing, Zhu, Di-Cheng, Li, Shi-Min, Cawood, Peter A., Wang, Rui-Qiang, Yi, Jian-Kang, Zhang, Liang-Liang, Xie, Jin-Cheng

    Published in Lithos (01-05-2024)
    “…The subduction geometry of the Neo-Tethyan oceanic lithosphere during the Early Cretaceous (i.e., shallow vs. steep subduction) remains in dispute due to the…”
    Get full text
    Journal Article
  3. 3

    Comparison of Surfactants Typically Used for Stabilizing Oil-in-Water Emulsions in Terms of Their Surface, Emulsifying, and in Vitro Digestion Properties by Xie, Meng-Fei, Qing, Chun, Banwell, Martin G., Yi, Jiankang, Chen, Yongle, Yang, Zhijian, Liang, Min-Yi, Lan, Ping

    Published in ACS food science & technology (18-10-2024)
    “…Emulsifiers play key roles in a number of industries including those concerned with the production of food, medicines and cosmetics. In the present study, the…”
    Get full text
    Journal Article
  4. 4

    Westward-younging high-Mg adakitic magmatism in central Tibet: Record of a westward-migrating lithospheric foundering beneath the Lhasa–Qiangtang collision zone during the Late Cretaceous by Yi, Jian-Kang, Wang, Qing, Zhu, Di-Cheng, Li, Shi-Min, Liu, Sheng-Ao, Wang, Rui, Zhang, Liang-Liang, Zhao, Zhi-Dan

    Published in Lithos (01-09-2018)
    “…Magmatic records with high Mg and low Y signatures provide important insights into the deep mantle dynamics that dictate the evolution of ancient orogenic…”
    Get full text
    Journal Article