机译:Mariana的岩浆管道系统在18度的玛丽安娜槽槽盆地盆地
Minist Educ Key Lab Submarine Geosci &
Prospecting Tech Qingdao 266100 Peoples R China;
Minist Educ Key Lab Submarine Geosci &
Prospecting Tech Qingdao 266100 Peoples R China;
Minist Educ Key Lab Submarine Geosci &
Prospecting Tech Qingdao 266100 Peoples R China;
Natl Oceanog Ctr Qingdao 266071 Peoples R China;
Shandong Inst Ocean Resources Explorat Qingdao 266555 Peoples R China;
Chinese Acad Sci Inst Deep Sea Sci &
Engn Sanya 572000 Peoples R China;
Minist Educ Key Lab Submarine Geosci &
Prospecting Tech Qingdao 266100 Peoples R China;
Minist Educ Key Lab Submarine Geosci &
Prospecting Tech Qingdao 266100 Peoples R China;
Mariana trough; Back-arc basin; Plagioclase; Thermobarometry; Magma evolution;
机译:Mariana的岩浆管道系统在18度的玛丽安娜槽槽盆地盆地
机译:活跃的弧后盆地火山岩浆管道和混合岩浆形成:东马努斯盆地北苏
机译:马里亚纳海槽的橄榄石:首先看一个活跃的弧后盆地下方的地幔
机译:马里亚纳弧后盆地的富金烟囱
机译:Backarc盆地伸展和地壳增生的构造和岩浆控制,来自Lau盆地和南马里亚纳海槽的见解。
机译:活跃中洋脊火山岩浆管道系统和地震活动性
机译:马里亚纳弧中部的沉积,火山和构造过程:马里亚纳海槽后弧盆地形成和西马里亚纳海岭