论文部分内容阅读
地裂运动是地壳运动的一种基本形式,是地壳与上地幔相互作用的结果。地裂运动与造山运动相对应是地球表面的主要造盆作用。地裂盆地是在引张力作用下的产物。世界上主要油气区和具开发前景的石油盆地大多与地裂运动有联系。基于油气的生成、运移、聚集、甚至开采都与地裂盆地的结构特征、成因机制、动力学过程及其发育演化息息相关,提出地裂盆地的初步分类方案有助于增进对含油气盆地的认识。
Earth-shaking movement is a basic form of crustal movement and is the result of the interaction between the crust and the upper mantle. Earth-shaking movement and orogeny corresponds to the main surface of the earth’s basin. Cracked basins are the product of tension. Most of the world’s major oil and gas fields and development prospects of oil basins are mostly associated with the movement of the earth. Based on the formation, migration, accumulation and even exploitation of oil and gas, which are closely related to the structural characteristics, genetic mechanism, dynamics and evolution of the fissured basins, it is suggested that the preliminary classification scheme of the fissured basins should be helpful to improve the hydrocarbon accumulation understanding.