Tectono-geochemistry and deep prospecting prediction in the Lekai lead-zinc deposit, Northwestern Guizhou Province, China

WAN Xin; HAN Runsheng; LI Bo; XIAO Xianguo; HE Zhiwei; WANG Jingteng; WEI Qingxi

doi:10.12029/gc20220613

GEOLOGY IN CHINA > 2022 > 49(6): 1875-1892. > DOI: 10.12029/gc20220613

WAN Xin, HAN Runsheng, LI Bo, XIAO Xianguo, HE Zhiwei, WANG Jingteng, WEI Qingxi. Tectono-geochemistry and deep prospecting prediction in the Lekai lead-zinc deposit, Northwestern Guizhou Province, China[J]. GEOLOGY IN CHINA, 2022, 49(6): 1875-1892. DOI: 10.12029/gc20220613

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Tectono-geochemistry and deep prospecting prediction in the Lekai lead-zinc deposit, Northwestern Guizhou Province, China

1.
Southwest Institute of Geological Survey, Geological Survey Center for Non-ferrous Mineral Resources, Kunming 650093, Yunnan, China
2.
Guiyang Mining Investment & Development Corporation. Ltd., Guiyang 550002, Guizhou, China
3.
Kunming Prospecting Design Institute of China Nonferrous Metals Industry Co., Ltd., Kunming 650051, Yunnan, China

Funds:

National Natural Science Foundation of China 41572060

National Natural Science Foundation of China U1133602

Yunling scholar project 2014

School-enterprise cooperation projects 20160039

projects for Yunnan Engineering Laboratory of Mineral Resources Prediction and Evaluation (YM lab) 2010

Yunnan Province Innovation Team 2012

More Information

Author Bio:
WAN Xin, male, born in 1993, master, engaged in mineral prospecting and exploration; E-mail: 782030310@qq.com
Corresponding author:
HAN Runsheng, male, born in 1964, senior researcher, supervisor of doctor candidates, engaged in the dynamics of tectonic ore- forming processes and prognosis of concealed deposits, economic geology; E-mail: 554670042@qq.com
Received Date: November 18, 2019
Revised Date: May 30, 2020
Available Online: September 25, 2023

Graphical Abstract

Abstract

Abstract

This paper is the result of mineral exploration engineering.
Objective
The Lekai lead-zinc deposit, located in the Pb-Zn deposit concentration of northwestern Guizhou, is one of the small-scale lead-zinc deposits newly discovered in recent years. Different from most lead-zinc deposits in the Pb-Zn deposit concentration of northwestern Guizhou, the Lekai lead-zinc deposit is controlled strictly by NE trending fault-fold structure, which is similar to most lead-zinc deposits in the Pb-Zn deposit concentration of northeastern Yunnan. The current research provided significant implications for the deep exploration in the Lekai lead-zinc deposit and the Sichuan–Yunnan–Guizhou Triangle area (SYGT).
Methods
This study applied a large deal of detailed structural analysis on mechanical properties for faults and folds in the mining area and tectono-geochemistry method.
Results
The results showed that duo-type and λ-type are the main ore-controlling structural styles in this area. Moreover, three tectonic associations have been divided, which are correspond to four tectonic systems, namely Hercynian to Mid Indosinian, Late Indosinian to Early Yanshanian, Mid-Late Yanshanian, and Himalayan epochs. The trace elements concentrations of tectonites represented three element associations of principal factors, including frontal halo elements (Sb-As-Hg) in low temperature ore-forming stage, mineralization-halo elements (Zn-Pb-Cd) in medium-low temperature ore-forming stage, and tail-halo elements (In-Sn-Ni-Cu) in medium temperature ore-forming stage.
Conclusions
In four tectonic systems, ore-forming tectonic system corresponded with Late Indosinian to Early Yanshanian. According to anomaly features and their distribution regularities, the possible migration direction of ore-forming fluid is from southwest to northeast, and six target prospecting areas have been put forward in the depth of mining.

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References (59)

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Tectono-geochemistry and deep prospecting prediction in the Lekai lead-zinc deposit, Northwestern Guizhou Province, China