摘要
澜沧江中段兰坪地区地处冈瓦纳大陆与扬子板块的拼接带部位,以昌宁构造混杂带(碧江断裂)为界划分为2个一级构造单元,其中昌都—普洱地块共划分出3个三级构造单元和4个四级构造单元。
The Lanping area of middle sector of Lancangjiang river belongs to the conjunction zone of Gondwana and Yangzi Plate, which can be divided into 2 tectonic units of order I, taking the Changning tectonic melange zone （ Bijiang fault） as the boundary. And the Changdu - Puer massif, one of the 2 tectonic units, can be further divided into 3 units of order 3 and 4 units of order 4.
出处
《云南地质》
2012年第4期512-515,共4页
Yunnan Geology
关键词
分划性构造
构造形迹
成生演化
构造混杂带
昌都-普洱地块
Division Structure
Structure Trace
Formation - Evolution
Tectonic Melange Zone
Chang-du - Puer Massif
