海洋地质与第四纪地质2012，Vol.32Issue(5)：57-66,10.DOI:10.3724/SP.J.1140.2012.05057
华南钦杭结合带东段成矿特征与构造背景
TECTONIC SETTINGS AND METALLOGENISM OF THE EASTERN SEGMENT OF THE QIN-HANG BELT,SOUTH CHINA
摘要
Abstract
The Qin-Hang Belt, an important metallogenic belt in South China, is situated in the junction of the Yangtze Block and the Cathaysia Block, bounded by the Jingdezhen-Xiangtan-Pingxiang Deep Fault Zone to the northwest of the Yangtze block and the Shaoxing-Xiangping-Beihai Deep Fault Zone to the southeast of Cathaysia Block. It has experienced the Jinning, Caledonian, Indosinian and Yanshanian movements successively, and suffered from oceanic subduction, continent-continent collision, formation of the South China Block, intensive intracontinental folding, Yanshanian reactivation, large-scale Mesozoic mag-matism and formation of intracontinental basins. Various mineral deposits controlled by correspondent structural patterns were formed in the belt in different periods, especially the Yanshanian Period.关键词
构造演化/成矿作用/燕山期/钦杭结合带Key words
the Qin-Hang Belt/tectonic evolution/metallogenism/Yanshanian分类
海洋科学引用本文复制引用
徐磊,李三忠,刘鑫,索艳慧,吴奇,王鹏程..华南钦杭结合带东段成矿特征与构造背景[J].海洋地质与第四纪地质,2012,32(5):57-66,10.基金项目
钦杭结合带(东段)多幕变形构造分析与成矿作用关系研究(20100733) （东段）
