rifting

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美

网络  裂谷系; 裂谷作用; 裂陷; 裂谷; 断裂作用

现在分词：rifting　

BNC.31905

双语例句

• Our observations are consistent with rifting, lithospheric thinning, and mantle upwelling in the region.
  研究结果表明与这些地区裂谷、岩石圈减薄和地幔上涌区相一致。
• These are proper rear boundaries of continental margins, the geodynamics of which are characterized by rifting on shelves, continental slopes, and marginal oceanic depressions.
  它们位于大陆边缘区的后缘，其地球动力学作用以大陆架、大陆斜坡和边缘海沉降区域的裂谷作用为特征。
• During rifting folding and inversion, gold-bearing metamorphic hydrothermal fluid and gold mineralization formed;
  在裂谷褶皱、回返期，形成含金变质热液，形成金矿化；
• Post rifting regional uplift resulted in low maturity of source rock and wide difference from each other.
  裂谷期后的区域抬升作用导致烃源岩的成熟度偏低，并且各断陷之间有机质的热演化程度相差悬殊。
• Discussion of Basin-fill Mechanism during Eogene Rifting Phase in Oujiang Trough, the East China Sea
  东海瓯江凹陷早第三纪裂谷期盆地充填机制探讨
• Qing-Yuan district is a granite-greenstone terrain, The greenstone was formed during the youth stage of massif rifting in late Archean.
  花岗岩形成巨大的岩体。清原地区是一个花岗&绿岩区，绿岩是在晚太古代年轻地体裂谷期形成。
• There are many rifting basins in the north margin;
  北部和西部边缘上发育着张性沉积盆地和走滑拉张盆地；
• From the Cretaceous Period to the Cenozoic Period, the volcanism was mainly related to the rifting;
  从白垩纪至新生代，火山作用主要与裂谷作用有关。
• NE China experienced regional rifting, post-rifting thermal subsidence and thermal reverse in Late Mesozoic.
  中国东北晚中生代经历了区域性的裂谷期、后裂谷热沉降期和反转期。
• Tectonic activities controlled basin type, subside central rifting, source rock distribution, oil and gas migration and accumulation as well. Furthermore, it controlled trap formation and petroleum distribution.
  研究区的构造活动不仅控制了沉积盆地类型和沉降中心的迁移，而且控制了烃源岩的分布、油气运移和聚集，还影响了圈闭的形成和油气分布。