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机译:从发散板块到会聚板块:奥陶纪期间沿中朝板块南缘和西缘产生的相移
Shandong Univ Sci & Technol, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Shandong, Peoples R China|Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266071, Shandong, Peoples R China;
Shandong Univ Sci & Technol, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Shandong, Peoples R China|Geocom Consultants, Valle Portet 17, Benitachell 03726, Spain;
China Petrochem Corp, Inst Petr Explorat & Prod, Beijing 100083, Peoples R China;
China Petrochem Corp, Inst Petr Explorat & Prod, Beijing 100083, Peoples R China;
Shandong Univ Sci & Technol, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Shandong, Peoples R China;
Shandong Univ Sci & Technol, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Shandong, Peoples R China;
China Petrochem Corp, Inst Petr Explorat & Prod, Beijing 100083, Peoples R China;
Sedimentary facies; Tectonic regime; Plate convergence; Ordovician; Sino-Korean plate; Plate margin;
机译:从分歧到会聚板:所产生的相片沿着奥陶诺迪亚中韩板块的南部和西方边缘转移
机译:收敛板缘现代锌-Ba-Pb矿床与不同板际Fe-Cu-Zn矿床的比较
机译:板块边缘和海洋沉积在发散和会聚的板块环境中(侏罗纪,Pelagonian区,NE Evvoia,希腊)
机译:智利北部西部Gondwana边缘的古生代板构造演变与阿根廷西北部
机译:阿拉斯加南部会聚板块边缘的平板俯冲,沉积盆地发育和油气系统的地球动力学。
机译:方丈冰架阿蒙森海大陆边缘的结构和西南极洲贝灵斯豪森板块向南的边界
机译:发散和收敛构造板材边缘地震性的比较 - 案例研究:红海和ZAGROS