前言众所周知,构造作用在盐类矿床形成过程中起着重要的控制作用。著名的盐矿地质学家博歇特(H. Borchert)虽然不承认区域构造条件对盐类沉积有决定性影响,但是他也不否认,对于巨厚的蒸发岩系来说,“其沉积确实有赖于气侯条件和构造运动的配合”。构造作用,特别是同生断层的形成和演化对中、新生代含油气盆地中油气藏形成和储集的影响,已为我国许多石油地质工作者所研究,取得了重要成果。袁见齐在总结我国碎 Foreword It is well known that tectonism plays an important controlling role in the formation of salt deposits. H. Borchert, a well-known salt mine geologist, does not admit that regional tectonic conditions have a decisive influence on the sedimentation of salt. Nor does he deny that for the thick evaporites, “its deposition really depends Coordination with climate conditions and tectonic movement. ” The tectonic effects, especially the formation and evolution of synsedimentary faults, have been studied by many petroleum geologists in the Meso-Cenozoic petroliferous basins and have achieved important results. Yuan see together in the summary of China’s broken