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bilateral subduction
相关语句
  双向俯冲
     According to the system analysis and study on stratigraphy and its chronology,lithofacies-paleogeograhy,basic-ultrabasic rocks,ophiolite suits,granide,zoning of paleontological geography,paleomagnetism,geophysics,telemeter and photo interpretation,ductile deformation and metamorphic belt,Kangguertag-Huangshan fault zone can be regarded as a collision zone of bilateral subduction in late Paleozoic era.
     据地层及其时代、岩相古地理、基性 -超基性岩及蛇绿岩套、花岗岩类、古生物地理区系、古地磁、地球物理、遥感影像及韧性变形变质带等系统分析研究 ,表明康古尔塔格 -黄山深断裂带为晚古生代双向俯冲对接碰撞带。
短句来源
  “bilateral subduction”译为未确定词的双语例句
     Kangguertag-Huangshan collision zone of bilateral subduction and its metallogenic model and prognosis in Xinjiang,China
     新疆康古尔-黄山对接碰撞带的存在、成矿模式及成矿预测
短句来源
  相似匹配句对
     7 in bilateral.
     胸水部位:左侧3,右侧20例,双侧7例。
短句来源
     Kangguertag-Huangshan collision zone of bilateral subduction and its metallogenic model and prognosis in Xinjiang,China
     新疆康古尔-黄山对接碰撞带的存在、成矿模式及成矿预测
短句来源
     Bilateral acoustic neuromas
     双侧听神经瘤
短句来源
     FLUIDS IN SUBDUCTION ZONES
     俯冲带的流体地质作用
短句来源
     ③subduction(O3-S);
     ③俯冲阶段(O3—S);
短句来源
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According to the system analysis and study on stratigraphy and its chronology,lithofacies-paleogeograhy,basic-ultrabasic rocks,ophiolite suits,granide,zoning of paleontological geography,paleomagnetism,geophysics,telemeter and photo interpretation,ductile deformation and metamorphic belt,Kangguertag-Huangshan fault zone can be regarded as a collision zone of bilateral subduction in late Paleozoic era. The north of it is Da'nanhu arc zone which belongs to the south edge of Kazakhstan-Junggar plate.The south...

According to the system analysis and study on stratigraphy and its chronology,lithofacies-paleogeograhy,basic-ultrabasic rocks,ophiolite suits,granide,zoning of paleontological geography,paleomagnetism,geophysics,telemeter and photo interpretation,ductile deformation and metamorphic belt,Kangguertag-Huangshan fault zone can be regarded as a collision zone of bilateral subduction in late Paleozoic era. The north of it is Da'nanhu arc zone which belongs to the south edge of Kazakhstan-Junggar plate.The south of it is part of Tarim plate.The Aqikekudouke-shaquanzi moved to the site of Kangguertag-Huangshan area in early Paleozoic era.It was pulled oppositely and then collided in Devonian and Carboniferous Period,and then solidified and rift partly in Permian Period.There is Qoltag Accretion Arc Zone between the plates where distributed volcanic rocks,basic-ultrabasic rocks,middle-acidic porphyry (porphyrite) and Au,Cu-Ni,Cu(Mo)ore deposits,which distributed over the bilateral subduction and collision zone.The distribution of the middle-acid porphyry(porphyrite) and Cu(Mo) ore deposits is symmetry.We built a model of regional tectonic-magma-metallization for metallogenic prognosis on the base of the fact.The model and prognosis have been tested and verified by the discovery of Chihu-Tuwu porphyry type Cu,Mo(Ag)ore deposit with reserve of 10 000 000 ton.It is important to the research of geological tectonics and ore prospect.

据地层及其时代、岩相古地理、基性 -超基性岩及蛇绿岩套、花岗岩类、古生物地理区系、古地磁、地球物理、遥感影像及韧性变形变质带等系统分析研究 ,表明康古尔塔格 -黄山深断裂带为晚古生代双向俯冲对接碰撞带。其南为塔里木板块 ,早古生代为库都克阿奇克 -沙泉子俯冲带 ;泥盆纪北移至康古尔塔格 -黄山一带 ,经泥盆 -石炭纪拉张、双向俯冲、对接碰撞 ,二叠纪固结 -裂解演化 ,两者间为觉罗塔格岛弧增生带 ;其北为哈萨克斯坦 -准噶尔板块南缘大南湖岛弧带 ;有基性 -超基性岩、火山岩和中酸性斑 (玢 )岩及铜镍、金和铜钼矿分布 ,中酸性斑 (玢 )岩及铜钼矿呈对称分布 ,进而建立区域构造 -岩浆 -成矿模式 ,进行战略性和战术性成矿预测。千万吨资源量的赤湖 -土屋斑岩型Cu、Mo(Ag)矿的发现 ,验证了这种模式和预测的正确性。对地质构造研究及找矿有重要意义。

 
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