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机译:大陆俯冲之前的持久海洋俯冲:大别造山带西部的海洋型高压榴辉岩的新Lu-Hf和Sm-Nd年代学
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China|Institute for Study of the Earth’s Interior, Okayama University, Tottori 682-0193, Japan;
School of Earth and Environmental Sciences, Washington State University, Pullman, Washington 99164, U.S.A.;
School of Earth and Environmental Sciences, Washington State University, Pullman, Washington 99164, U.S.A.;
Institute for Study of the Earth’s Interior, Okayama University, Tottori 682-0193, Japan;
CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China;
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;
机译:大陆俯冲之前的长时间海洋俯冲:大别造山带西部的海洋型高压榴辉岩的新Lu-Hf和Sm-Nd年代学
机译:新的Lu-Hf和Sm-Nd年代学约束了大别造山带石炭-二叠纪期间大洋地壳俯冲
机译:大别造山带海洋俯冲到大陆俯冲的过渡时间:U-Pb,Lu-Hf,Sm-Nd和Ar-Ar多重计时测年的约束
机译:大洋俯冲-陆相碰撞过渡与超热金矿化:西天山图拉苏矿团塔吾尔别克矿床年代学研究的启示
机译:华南地块的碰撞,旋转及可能的俯冲撤离:对中国大别山造山带高压(HP)和超高压(UHP)变质岩的挖掘的意义
机译:PNAS Plus:从高精度地球年代学推断海洋扩散中心可以快速转换为俯冲带
机译:西部山脉潘帕那亚斯山脉:漫长的格林维尔时代(1330–1030 Ma) ud海洋弧线,大陆边缘俯冲增生和AMCG ud板内岩浆作用