The Geological Evolution and Metallization of Talas-Kalatawu Block in Northern Tianshan, Kyrgyzstan
详细信息
- 责任者：Fan Baocheng (Xi’an Center of Geological Survey ; China Geology Survey ; Xi’an 710054 ; China) ; Meng Guanglu
- 刊名：Northwestern Geology
- 出版年：2013
- 卷期：46(2)
- 关键词：含矿建造 ; ore-bearing formations ; 吉尔吉斯斯坦 ; Kyrgyzstan
- 页码：p.54-62
- 图表：4 illus., 1 table, 32 refs.
- 分类号：1000
- issnNo：ISSN1009-6248
- isbnNo：CN61-1149/P
摘要
Talas-Kalatawu block is composed of Malakaluoyi terrane, Guokejiaote terrane and Wuzunahama’te terrane. According to the mineral-bearing formation and distribution of ore deposits and spots, the Block can be divided to four polymetallic mineralization belts. Long-term tectonic evolution and magmatic activity lead to the mineralization stacking in this field, however, the metallization is mainly formed by collision and extrusion magmatism in the late period of Caledonian orogeny.