Tectonic Evolution and Metallogenesis of
详细信息
- 责任者：Dong Lianhui (Bureau of Geology and Mineral Resources Development of Xinjiang ; Urumqi 830011 ; China) ; Qu Xun
- 刊名：Xinjiang Geology
- 出版年：2010
- 卷期：28(4)
- 关键词：构造演化 ; structural evolution ; 成矿作用 ; metallogenesis ; 新疆 ; Xinjiang
- 页码：p.351-357
- 图表：4 illus., 67 refs.
- 分类号：1001
- issnNo：ISSN1000-8845
- isbnNo：CN65-1092/P
摘要
Tectonics of Xinjiang shows "five blocks and four belts" pattern. Siberia, Kazakhstan-Junggar,Tarim-North China, South China and Tibet blocks was divided by four belts that is Charles-Qiaoxiahala-Buergen, Nalati–Hongliuhe, Kangxiwa-Jingyuhu, and Aksai Chin-Gold Sand River. The plates have experienced four evolution stages that include the continental nucleus, continental block, margins and intra-continental stage. As a result of different evolutionary stages of mineralization, it appears different mineral characteristics. For example, around Tarim Basin mainly including strata-bound iron, lead, zinc, copper, gold deposits, around Junggar mainly include porphyry, mafic-ultramafic magmatic, volcanic rock-type copper-molybdenum, nickel, chromium, gold and other minerals.
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