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机译:大巴山前陆带构造驱动的有机流体运移:以地球化学和地热法为依据,证实了脉状充填方解石纤维的有机包裹体
School of Earth Science and Land Resources. Chang'an University, Xi'an, Shannxi Province 7W054, PR China,Key Laboratory of West Mineral Resource & Geology Engineering, Education Ministry of China, Chang'an University, Xi'an, Shannxi Province 710054, PR China;
Chinese Academy of Geological Sciences, Beijing 10003, PR China;
Geoscience Department, Trinity University, San Antonio, TX 78212, USA;
School of Earth Science and Land Resources. Chang'an University, Xi'an, Shannxi Province 7W054, PR China,Geoscience Department, Trinity University, San Antonio, TX 78212, USA;
Hydrocarbons; Fibrous calcite; Fluid inclusions; Dabashan Fold Belt; China;
机译:中国中部大巴山褶皱冲断带南部的流体流动事件:方解石脉中流体包裹体和同位素数据的启示
机译:中国中部南部大巴山褶皱冲断带的流体流动事件:方解石脉中流体包裹体和同位素数据的启示
机译:大巴山前陆冲断带古流体的起源:脉状和宿主岩中13C,18O和87Sr / 86Sr的地球化学证据
机译:中国中部大巴山前陆有机流体的迁移
机译:前陆褶皱带中的透明度液体迁移:来自Sevier折叠带的Wyoming突出的证据
机译:陶艺工人支气管肺泡灌洗液中的非纤维状无机颗粒。
机译:构造和天然液体迁移对前陆褶皱腰带储层进化的发病率和重要性
机译:地质学,热液岩石学,稳定同位素地球化学和流体包裹体地温测定法LasL地热测试井C / T-1(mesa 31-1),East mesa,Imperial Valley,California,Usa