Skip to main content

and
  1. No Access

    Article

    Influence of Mn–Si elements on the kinetics of oxidative phase transformation under continuous cooling conditions and modeling study

    In this paper, a simultaneous thermal analyzer carried out isothermal eutectoid transformation experiments of Fe–0.4Mn, Fe–1.2Mn, and Fe–1.2Mn–0.2Si alloys. The kinetic model of the isothermal phase transforma...

    Guangming Cao, Wencong Zhao, Wentao Song, Hengxiang Yu in Journal of Materials Science (2024)

  2. No Access

    Chapter and Conference Paper

    Geochronological and geochemical study on the Yulong porphyry copper ore belt in eastern Tibet, China

    The Yulong copper belt, along part of the Red River-Ailao Shan fault system and its northwestern extension in eastern Tibet, consists of five porphyry pipes that contain a total copper resource of over 8 milli...

    Huaying Liang, Yuqiang Zhang, Yingwen **e in Mineral Deposit Research: Meeting the Glob… (2005)

  3. No Access

    Article

    PGE geochemistry of Jiding ophiolite in Tibet and its constraint on mantle processes

    The total PGE amount (σPGE) of mantle peridotite in the Jiding ophiolite is slightly higher than that of the primitive mantle, but the PGE contents of basalt are higher than those of the mid-ocean ridge basalt...

    Bin **a, Genwen Chen, Houjun Mei, Lingzhi Guo in Science in China Series D: Earth Sciences (2001)

  4. No Access

    Article

    Platinum-group elements for the mantle peridotites in the Dazhuka ophiolite, Tibet, China

    The total PGE amounts of mantle peridotites in the Dazhuka ophiolite, Tibet, are 28.37–50.67 ng/g, slightly higher than those of mantle peridotites in the primitive mantle, and typical ophiolites in the world,...

    Hengxiang Yu, Bin **a, Houjun Mei, Linzhi Guo, Liang Qi in Chinese Science Bulletin (2001)

  5. No Access

    Article

    The metallogenic mechanism of the sandstone-type copper deposits in the Chuxiong Basin, Yunnan Province

    The sandstone-type Cu deposits in the Chuxiong Basin occur in the Cretaceous Gaofengsi Formation and the Maotoushan Formation and the orebodies are stratoid and lenticular in form, structurally controlled by t...

    Genwen Chen, Bin **a, Yanzhi Wu, Guangzhi Tu in Science in China Series D: Earth Sciences (2000)