CAJ | 학술논문

提20世纪60年代板块构造学说传入中国，为广大地学工作者所接受并应用于相关的地质工作中。在新一代地质志的研究中，以板块学说为主导，已经成为共识。从板块构造来认识，板块的组成包括其核心及边缘。其核心为克拉通，由稳定的陆块组成；边缘包含了不同的活动大陆边缘和被动大陆边缘。边缘在后期板块汇聚的过程中，常由汇聚或碰撞等不同方式而成为不同的造山带。板块之间具有不同形式的汇聚带，其中主要是地壳对接消减带。在地球发展历史的过程中，不同时期的板块构造格局常有很大的变化。因此，本文以古生代的构造格架为主，探讨对中国大陆进行板块构造区划中的一些相关问题，并对全国的区划提出了一个初步方案。此方案将全国划分为7个I级单元（板块），30个II级单元（克拉通和造山带）以及103个III级单元。
제20세기60년대판괴구조학설전입중국，위엄대지학공작자소접수병응용우상관적지질공작중。재신일대지질지적연구중，이판괴학설위주도，이경성위공식。종판괴구조래인식，판괴적조성포괄기핵심급변연。기핵심위극랍통，유은정적륙괴조성；변연포함료불동적활동대륙변연화피동대륙변연。변연재후기판괴회취적과정중，상유회취혹팽당등불동방식이성위불동적조산대。판괴지간구유불동형식적회취대，기중주요시지각대접소감대。재지구발전역사적과정중，불동시기적판괴구조격국상유흔대적변화。인차，본문이고생대적구조격가위주，탐토대중국대륙진행판괴구조구화중적일사상관문제，병대전국적구화제출료일개초보방안。차방안장전국화분위7개I급단원（판괴），30개II급단원（극랍통화조산대）이급103개III급단원。
Since the 1960’s,the plate tectonic theory has been widely Prevailing in China. Having been popularly adopted by Chinese geologists, this theory has been applied to different related fields. In the work of new“regional geology”, it has become the dominant idea. The theory of plate tectonics argues that a plate is formed by its core and its margins. Its core is a craton usually made of stable continental massif, whereas its margins include different active and passive continental margins. In the process of convergence of plates, the continental margins became different orogenic belts through their different convergences and collisions. There are different convergent zones between plates, among which the Convergent Crustal Consumption Zone is dominant. In the historical process of crustal development, huge changes of the plate tectonic framework took place. Based on the plate tectonic framework of Paleozoic, the authors discussed some problems concerning the regional subdivicion of China and suggested a tentative plan for regional subdivicion of China in this paper. According to the plan, China is divided into 7 first class units (plates), 30 second class units (cratons and orogenic belts) and 103 third class units.