机译:青藏高原东北部隆起引起西宁盆地中新世早期早期干旱化加剧的证据
Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China;
China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China;
Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China;
Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China;
Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China;
Inner Asia; Early Miocene; Clay minerals; Acidification; Tibetan Plateau uplift;
机译:晚期内部强化构造隆起和气候充气在东北藏高原:来自西宁盆地的粘土矿物学和地球化学记录的证据
机译:晚期内部强化构造隆起和气候充气在东北藏高原:来自西宁盆地的粘土矿物学和地球化学记录的证据
机译:西宁盆地沉积档案中青藏高原东北隆起在25-20Ma之间的证据
机译:西藏高原东北边界六山山隆起的地位论证证明
机译:在新生代藏高原藏边缘的构造与气候之间的相互作用:西藏高原和西北地区西北地区的案例研究促进了自新世纪以来中纬度亚洲