论构造复合

ON COMPOUNDING TECTONICS

构造复合现象在地壳岩石圈中普遍存在，它是构造运动多期次多阶段发展的记录。构造复合存在多种多样的形式，其基本形式不仅包括各种形迹的复合，建造与形迹的复合，而且包括建造与建造的复合；就其复合的空间位置而言，既有原地的复合，也有异地的复合；就运动方式而言，既有同方式运动的复合，也有不同方式运动的复合；就构造复合的规模和等级而言，小至小型或显微构造，中至露头规模的构造形迹复合，大至构造带、构造地块、构造体系乃至巨型构造域（岩石圈板块）的复合。文章特别强调了复合构造域和区域构造体系等概念。用三大板块相互作用和构造复合的概念解释了存在于我国及其邻区的区域构造体系的形成机制。文章的最后提出了构造复合的若干基本规律。

Tectonic compounding common in the earth crust and lithosphere is the records of repeated tectonic movements.There is a great variety of tectonic compounding the basic types of which include the compounding of various structural features, and that between structural features and geological formations as well as that of various geological formations.The compounding structures may be either autochthonous or allochthonous;they may also comprise structural features caused by the same manner of tectonic movements or by different manner of tectonic movements;and finally,there may be compounding of structures of all sizes ranging from microscopic ones up to tectonic belts or even tectonic domains. The author emphasizes the concepts of compounding tectonic domains and regional tectonic systems.These concepts have been used to explain the mechanism of the formation of regional tectonic systems in China and adjacent areas.