|Table of Contents|

Geological Characteristics, Genetic Types and Metallogenic Regularity of Indosinian Deposits in East Tianshan, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2023年第03期
Page:
590-621
Research Field:
基础地质与矿床地质
Publishing date:

Info

Title:
Geological Characteristics, Genetic Types and Metallogenic Regularity of Indosinian Deposits in East Tianshan, China
Author(s):
DENG Xiao-hua1*;  WU Chang-zhi1;  WU Yan-shuang2;  CHEN Xi3;  ZHANG Jing4;  SHI Yu5;  CHEN Yan-jing2; 6**
(1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Xinjiang Mineral Resources Research Center, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, Xinjiang, China; 3. School of Earth Sciences and Engineering, Sun Yat-sen University, Zhuhai 519080, Guangdong, China; 4. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 5. State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, Jiangxi, China; 6. Key Laboratory of Orogenic Belts and Crustal Evolution of Ministry of Education, Peking University, Beijing 100871, China)
Keywords:
geological characteristic;  deposit type;  ore-controlling factor;  metallogenic regularity;  Indosinian;  tectonic setting;  East Tianshan;  Central Asian orogenic belt
PACS:
P61
DOI:
10.19814/j.jese.2023.03056
Abstract:
East Tianshan metallogenic belt, which is one of the important metallogenic belts in China, is characterized by large-scale mineralization during Paleozoic. In recent years, a number of Indosinian age data have been reported in East Tianshan metallogenic belt, which have attracted a lot of attention. The geological characteristics, genetic types and metallogenic regularity of Indosinian deposits in East Tianshan were summarized. The results show that Indosinian deposits in East Tianshan contain not only large-superlarge scale Au, Mo, W, Re, and Rb deposits, but also Li, Be, Nb, Ta, V, Ti, Fe and other metal deposits, indicating the importance of Indosinian mineralization in East Tianshan. The genetic types of Indosinian deposits include magmatic deposits, i.e., magmatic V-Ti magnetite deposit, granite-type Rb deposit and pegmatite-type Li-Be-Nb-Ta deposit, and hydrothermal deposits, i.e., porphyry-type Mo-Re deposit, skarn-type W-Mo-Rb deposit, quartz vein-type W deposit, orogenic-type and epithermal-type Au deposits. Indosinian deposits in East Tianshan are mainly distributed in Kanggu'er ductile shear zone, Central Tianshan terrane, and their southeastern margin, but there is little metallogenic information in other tectonic units. The distribution of Indosinian deposits is similar in time and space, but the key ore-controlling factors are obviously different. Skarn-type W deposit is obviously controlled by Precambrian basement of Central Tianshan terrane; V-Ti magnetite deposit, granite-type Rb deposit, pegmatite-type Li-Be-Nb-Ta deposit and porphyry-type Mo deposit are controlled by different intrusive rocks; and orogenic-type Au deposit is obviously controlled by ductile shear zone and fault structure. Therefore, the resource potential of Indosinian orogeny in East Tianshan has been preliminarily shown, and more attention should be paid to the study on Indosinian mineralization and ore exploration in East Tianshan and even Xinjiang in the future.

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Last Update: 2023-05-30