Metallogenic regularity and prospecting direction of Tin deposits in North China

TIAN Jie-peng; LI Junjian; ZHANG Tong; FU Chao; DANG Zhi-cai; HE Jiang-tao; ZHANG Peng-peng

doi:10.19948/j.12-1471/P.2023.01.02

2023 Vol. 46, No. 1

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TIAN Jie-peng, LI Junjian, ZHANG Tong, FU Chao, DANG Zhi-cai, HE Jiang-tao, ZHANG Peng-peng. 2023. Metallogenic regularity and prospecting direction of Tin deposits in North China. North China Geology, 46(1): 20-26. doi: 10.19948/j.12-1471/P.2023.01.02

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TIAN Jie-peng, LI Junjian, ZHANG Tong, FU Chao, DANG Zhi-cai, HE Jiang-tao, ZHANG Peng-peng. 2023. Metallogenic regularity and prospecting direction of Tin deposits in North China. North China Geology, 46(1): 20-26. doi: 10.19948/j.12-1471/P.2023.01.02

Metallogenic regularity and prospecting direction of Tin deposits in North China

1. Key Laboratory of Building Structural Retrofitting and Underground Space Engineering of Ministry of Education, Jinan 250101, China;
2. School of Civil Engineering, Shandong Jianzhu University, Jinan 250101, China;
3. Key Laboratory of Gold Mineralization Processes and Resource Utilization Subordinated to the Ministry of Land and Resources, Key Laboratory of Metallogenic Geological Process and Resources Utilization in Shandong Province, Jinan 250013, China;
4. Tianjin Center, China Geological Survey, Tianjin 300170, China;
5. Geological Survey Institute of Inner Mongolia Autonomous Region, Hohhot 050081, China;
6. Institute of Geophysical and Geochemical Exploration of Chinese Academy of Geological Science, Langfang 065000, China;
7. Hebei GEO University, Shijiazhuang 050031, China

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Corresponding author: LI Junjian

Received Date: 30 December 2021

Abstract

Abstract

Tin resources are abundant in North China, especially in the middle and southern Greater Khingan Range, which is one of the three major tin mining areas in our country and the only formed tin polymetallic ore belt found in the north of China.The types of tin deposits in North China are mainly divided into three categories: hydrothermal, porphyry and contact account type, most of which are co-occurring and associated deposits, with few independent tin deposits.The mineralization period of tin deposits in the region is mainly concentrated in the Late Jurassic-Early Cretaceous.On this basis, the main ore-controlling factors of tin deposits in North China were analyzed, the metallogenic models of contact metasomatic, porphyry and hydrothermal tin deposits were initially established, and the temporal and spatial distribution of tin deposits were discussed, and Xilinhot-Keshiketeng Banner, Erlian-Dongwu Banner and Shangdu-Taipusi Banner are key areas for searching for tin deposits in North China.
- contact metasomatic type /
- hydrothermal type /
- porphyry type /
- metallogenic model /
- prospecting direction /
- tin deposits /
- North China

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