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SHI Yonghong, WANG Yong, CHEN Bailin, TAN Renwen, GAO Yun, SHEN Jinghui. 2022. Characteristics of silicon-calcium surface ore-controlling in Fengtai ore-concentration areas, West Qinling Mountains: Examples from Qiandongshan Pb-Zn deposit[J]. Geology in China, 49(1): 226-240. doi: 10.12029/gc20220114
Citation: SHI Yonghong, WANG Yong, CHEN Bailin, TAN Renwen, GAO Yun, SHEN Jinghui. 2022. Characteristics of silicon-calcium surface ore-controlling in Fengtai ore-concentration areas, West Qinling Mountains: Examples from Qiandongshan Pb-Zn deposit[J]. Geology in China, 49(1): 226-240. doi: 10.12029/gc20220114
shu

Characteristics of silicon-calcium surface ore-controlling in Fengtai ore-concentration areas, West Qinling Mountains: Examples from Qiandongshan Pb-Zn deposit

  • 1.

    Laboratory of Dynamic Digenesis and Metallogenesis, Institute of Geomechanics, CAGS, Beijing 100081, China

  • 2.

    China University of Geoscience (Beijing), Beijing 100083, China

  • 3.

    China University of Geoscience (Wuhan), Wuhan 430074, Hubei, China

    • Fund Project: Supported by the project of China Geological Survey (No.DD20160053), Fundamental Research Funds of Central Welfare Research Institutes, CAGS (No. JYYWF20183702, No. JYYWF20180602)
More Information
  • Author Bio: SHI Yonghong, male, born in 1986, master, majors in geological engineering; E-mail: 1075638571@qq.com
  • Corresponding author: WANG Yong, male, born in 1982, senior engineer, mainly engaged in the study of ore deposits and geochemistry; E-mail: wangyong429@163.com 
Received Date:  17 October 2019
Revised Date:  25 December 2019
Publish Date:  25 February 2022
    Abstract

  • This paper is the result of mineral exploration engineering.

     Objective

    The Fengtai ore-concentration area in the Western Qinling is an important part of the Qinling lead-zinc-gold polymetallic metallogenic belt. However, there has been a long running controversial debate about the type and ore-controlling factors of the lead-zinc ore-concentration area.

     Methods

    Based on the detailed field investigation and data combing of the representative Qiandongshan lead-zinc deposit in the Fengtai ore-concentration Area, the ore-controlling characteristics of the silicon-calcium surface of the deposit are discussed.

     Results

    It is considered that the bottom plate of the c in the Fengtai Basin is the limestone of the Gudaoling Formation, which is analkaline calcareous rock, and the top plate is the phyllite of the Xinghongpu Formation, which is a siliceous rock. They form a perfect Si/Ca interface. The initially enriched ore-forming materials in the stratumwere enriched again under the action of the Triassic magmatic hydrothermal fluid, andmigrates along a series of NWW-strikefold structures and syngeneic faults in the basin, therefore, they concentrate to form deposits at the Si/Ca interfaceof the turning end of large folds, interlayer slip zone, etc.

     Conclusions

    Based on this, it is considered that the interlayer slip zone near the turning end of the compound anticline and its wings, the saddle portion of the interticle, and the interlayer slip zone in the area are favorable areas for mineralization.At the same time, the metallogenesis of the Indosinian lead-zinc deposit in the Western Qinling was coupled with large-scale tectonic-magmatic activities in space and time. And the types of lead-zinc deposits in the ore-concentrated area are hydrothermal deposits related to magmatic activities.
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