地裂运动

峨眉地裂运动和四川盆地天然气勘探实践

Emei Taphrogenesis and Natural Gas Prospecting Practices in Sichuan Basin

略论地裂运动与中国油气分布

A discussion of taphrogenesis and hydrocarbon distribution in China

这与兴凯地裂运动早期的构造热流体活动有着紧密的相关性。

The hydrothermal fluid has been related to the early Xingkai taphrogenesis thermal activity .

试论上扬子地台的峨眉地裂运动

On Emei taphrogenesis of the upper Yangtze Platform

中国地裂运动观的创建和发展

Establishment and development of Chinese taphrogeny outlook

四川盆地西部的峨眉地裂运动及找气新领域

The Emei taphrogenesis and the new regions for searching gas in the western part of Sichuan Basin

四川盆地下二叠统白云岩及古岩溶的形成与峨眉地裂运动的关系

The formation of dolomite and paleokarst of the lower Permian Series in Sichuan Basin and the relation to the Emei taphrogenesis

后经“峨嵋地幔柱”的作用和二叠纪“峨嵋地裂运动”的拉张，“塔里木&扬子古大陆”裂解、分离。

Under the action of " Emei mantle plume " and the extension of " Emei Taphrogeny ", the Tarim-Yangtze Paleocontinent diverged and separated .

地裂运动形成的构造格局对沉积、成岩有一定的控制作用，进而在一定程度上控制了该区油气的分布。

The structural framework , formed by Emei Taphrogenesis , controlled the sedimentation and diagenesis , thus more or less controlled the distribution of hydrocarbon in the area .

地裂带空间位置和地裂的运动受构造活动控制，而地下水的过量开采和强降雨过程又影响地裂发生的时间、地段和发育程度。

The space location and the fissure movement of the ground fissure belt are controled by the tectonic movement , and the occurrence time and the development stage are influenced by the overexploitation of the underground water and the strong precipitation process .