CAJ | 학술논문

贵州地处特殊构造部位和地史时期经历了多次构造活动和多种地质事件，使贵州由活动陆缘一被动陆缘一陆块内部转化；由准大洋型地壳（红海型）一过渡型地壳一大陆型地壳转化；地壳由活动一稳定转化；地壳厚度由薄一厚转化，地壳结构可划分为三层，地壳发展与演化划分为四阶段。因此，贵州地壳具有多层性、地壳发展与演化具有多期多阶段的特点，大地构造单元可分为“一块两带”，即上扬子陆块、江南造山带和右江造山带。
귀주지처특수구조부위화지사시기경력료다차구조활동화다충지질사건，사귀주유활동륙연일피동륙연일륙괴내부전화；유준대양형지각（홍해형）일과도형지각일대륙형지각전화；지각유활동일은정전화；지각후도유박일후전화，지각결구가화분위삼층，지각발전여연화화분위사계단。인차，귀주지각구유다층성、지각발전여연화구유다기다계단적특점，대지구조단원가분위“일괴량대”，즉상양자륙괴、강남조산대화우강조산대。
Situated in a special tectonic position, and experienced tectonic movements and geological events, Guizhou belongs to a special geohistory period which makes Guizhou transfer from active continental margin and passive continental margin to inner land mass, from pre-continental crust and transitional crust to continental crust, and makes the crust stable and thicker. The crust can be divided into 3 layers and the crust development and evaluation can be divided into 4 periods. So the crust in Guizhou has multi-layers and the crust development and evaluation has multi periods. The plate tectonic can be divided in to one block and two zones： Upper Yangtze land mass, Jiangnan orogenic belt and Youjiang orogenic belt.