The Geological Evolution and Metallization of Talas-Kalatawu Block in Northern Tianshan,Kyrgyzstan

FAN Bao-cheng; MENG Guang-lu; WANG Bin; CAO Ji-fei; LI Hui-ying; ZHANG Jing; CAO Xin

Northwestern Geology > 2013 > 46(2): 54-62.

FAN Bao-cheng, MENG Guang-lu, WANG Bin, et al. The Geological Evolution and Metallization of Talas-Kalatawu Block in Northern Tianshan,Kyrgyzstan[J]. Northwestern Geology, 2013, 46(2): 54-62.

Citation:

FAN Bao-cheng, MENG Guang-lu, WANG Bin, et al. The Geological Evolution and Metallization of Talas-Kalatawu Block in Northern Tianshan,Kyrgyzstan[J]. Northwestern Geology, 2013, 46(2): 54-62.

Citation:

FAN Bao-cheng, MENG Guang-lu, WANG Bin, et al. The Geological Evolution and Metallization of Talas-Kalatawu Block in Northern Tianshan,Kyrgyzstan[J]. Northwestern Geology, 2013, 46(2): 54-62.

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The Geological Evolution and Metallization of Talas-Kalatawu Block in Northern Tianshan,Kyrgyzstan

Xi'an Center of Geological Survey, China Geology Survey Xi'an Shaanxi 710054, China

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Received Date: December 17, 2012
Revised Date: January 17, 2013
Published Date: June 04, 2013

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Abstract

Talas-Kalatawu block is composed of Malakaluoyi terrane, Guokejiaote terrane and Wuzunahama'te terrane. The southern boundary of Talas-Kalatawu block is Taras-Fergana dextral strike-slip fault, and adjacent to Mid-Tianshan; the northern boundary is Suzaq-Yiqigelietawu-Alamu Zoe fault, and adjacent to North Tianshan. The three tectonic units varies from one another due to their sedimentary formation in different geological periods. 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.
- Taras-Kalatawu,
- sedimentary formation,
- mineral-bearing formation,
- collision and extrusion

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The Geological Evolution and Metallization of Talas-Kalatawu Block in Northern Tianshan,Kyrgyzstan

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