Relationship between Jinshajiang-Honghe strike-slip fault and Cu-Au polymetallic mineralization of alkaline-rich porphyry

WANG Jianhua; LI Wenchang; HE Wenyan; MI Yunchuan

doi:10.12029/gc20200703001

GEOLOGY IN CHINA > 2023 > 50(5): 1542-1556. > DOI: 10.12029/gc20200703001

WANG Jianhua, LI Wenchang, HE Wenyan, MI Yunchuan. Relationship between Jinshajiang-Honghe strike-slip fault and Cu-Au polymetallic mineralization of alkaline-rich porphyry[J]. GEOLOGY IN CHINA, 2023, 50(5): 1542-1556. DOI: 10.12029/gc20200703001

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Relationship between Jinshajiang-Honghe strike-slip fault and Cu-Au polymetallic mineralization of alkaline-rich porphyry

1.
Research Center of Natural History and Culture, Qujing Normal University, Key Laboratory of Yunnan Province Universities of Qujing Natural History and Early Vertebrate Evolution, Qujing 655011, Yunan, China
2.
Faculty of Land and Resource Engineering, Kunming University of Science and Technology, Kunming 650093, Yunnan, China
3.
State Key laboratory of Geological Processes and Mineral Resource, China University of Geosciences, Beijing 100083, China
4.
Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China

Funds:

Basic Research Special Youth Project of Yunnan Province 202001AU070145

the State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS) 213117

More Information

Author Bio:
WANG Jianhua, born in 1987, senior engineer, mainly engaged in regional metallogeny and stratigraphy research; E-mail: wjhmessi@163.com
Received Date: July 02, 2020
Revised Date: October 07, 2020
Available Online: November 17, 2023

Graphical Abstract

Abstract

Abstract

Objective
This paper is the result of mineral exploration engineering.
Objective
The Jinshajiang-Honghe alkaline-rich porphyry Cu-Au polymetallic metallogenic belt, which produces numbers of large-scale Cu-Au deposits including the Yulong at the north, the Beiya in the middle and the Tongchang at the south, for example, has becoming one of the most productive ore clusters and research focus in the east Tethys domain.
Methods
Based on long-term integrated field investigations and published data analysis, we summarized the characteristics of the typical deposits and the alkaline-rich porphyry.
Results
The alkaline-rich porphyry mainly consists of monzonitic granite porphyry and quartz syenite porphyry, showing high contents of K₂O-Na₂O, Al₂O₃, LREE and deficit in HREE and HFSE. Similar Sr-Nd isotopic composition indicates that the source area is mainly lower crust material. The development characteristics of regional strike-slip structures and their constraints on diagenesis and mineralization in this area are also discussed, and a "regional structure→alkaline-rich magma→Cu-Au polymetallic" mineralization process controlled by the deep Jinshajiang-Honghe strike-slip fault and its secondary structure activities in the east Tethys metallogenic domain is further summarized.
Conclusions
Through field observation and study on the main faults in the three typical areas, we suggest that the alkaline-rich magma and related Cu-Au mineralization were primarily controlled by the secondary northwestward faults of the regional Jinshajiang-Honghe strike-slip fault.

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References (106)

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Relationship between Jinshajiang-Honghe strike-slip fault and Cu-Au polymetallic mineralization of alkaline-rich porphyry