走滑构造研究进展

Progress in research of strike-slip tectonics

胡德胜 佟殿君 阳怀忠

中国地质大学资源学院，湖北 武汉 430074

Faculty of Resources, China University of Geosciences, Wuhan 430074, China

作为地球上一种重要的构造类型，走滑构造的研究意义并不亚于碰撞构造和伸展构造，但总体上其研究程度相对较低。在阅读大量中外文献的基础上，回顾了走滑构造的研究历程并系统总结了研究现状和进展，概述了各种先进的测试手段与勘探技术的应用。中国大陆广泛发育的大型走滑断裂带，相关人员已做了大量的研究工作。文中阐述了发育于中国东部和西部的大型走滑断裂带——郯庐断裂带、红河断裂带和阿尔金断裂带的活动时间、演化过程及其对盆地发育和演化的控制。实践证明，加强对走滑构造带的研究，有利于油气勘探总体水平的提高。同时，深入研究走滑构造所形成的相关构造，有助于更全面地研究造山带和盆地的构造演化过程，为古地理及地震灾害等应用领域提供了理论指导。

As one of the most important tectonic types, the research significance of strike-slip tectonics is no less than collision and extension tectonics,but the research degree is relative low. Based on a large amount of Chinese and foreign literatures,this article reviews the research history, analyzes the current research situation and progress for strike -slip tectonics, summarizes the application of various advanced test measures and exploration techniques. Previous scholars have done lots of research on the strike-slip tectonics developed widely in Chinese mainland. The article describes the activity time, evolutionary process of large
strike-slip faulted zones, namely Tanlu faulted zone, Red River faulted zone and Aerjin faulted zone, and their controlling on basin development and evolution in the east and the west of China. Practice shows that strengthening study of strike-slip tectonic zone is favorable for the improvement of petroleum exploration. At the same time, the research of relative structure formed by strike-slip techtonics is helpful for understanding the evolutionary process of basin and orogenic belt, which provides a theoretic guide for the research of palaeogeography and earthquake disaster.