Zircon U-Pb age, geochemistry and genesis of acid intrusive rocks in the Yuejinshan skarn type copper-gold deposit, Wandashan block

ZHANG Guobin; HAN Chao; YANG Yanchen; LIANG Bing; WEI Yanlan; HAN Shijiong

doi:10.12029/gc20180507

GEOLOGY IN CHINA > 2018 > 45(5): 977-991. > DOI: 10.12029/gc20180507

ZHANG Guobin, HAN Chao, YANG Yanchen, LIANG Bing, WEI Yanlan, HAN Shijiong. Zircon U-Pb age, geochemistry and genesis of acid intrusive rocks in the Yuejinshan skarn type copper-gold deposit, Wandashan block[J]. GEOLOGY IN CHINA, 2018, 45(5): 977-991. DOI: 10.12029/gc20180507

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Zircon U-Pb age, geochemistry and genesis of acid intrusive rocks in the Yuejinshan skarn type copper-gold deposit, Wandashan block

1.
Department of Geology, Liaoning Technical University, Fuxin, 123000, Liaoning, China
2.
Department of Mechanics and Engineering Science, Liaoning Technical University, Fuxin, 123000, Liaoning, China
3.
College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China
4.
Institute of Karst Geology, CAGS, Guilin 541004, Guangxi, China

Funds:

China Geological Survey Program 1212011120342

China Geological Survey Program 1212010786005

Doctor Scientific Research Foundation of Liaoning Province 201601370

The Sixth Agricultural Technology Problems Foundation of Liaoning Technical University 20160084T

More Information

Author Bio:
ZHANG Guobin, born in 1983, doctor, lecturer, majors in mineral resource prospecting and exploration, deposit and mineral exploration; E−mail: zhangguobin000@163.com
Received Date: July 08, 2016
Revised Date: November 02, 2016
Available Online: September 25, 2023

Graphical Abstract

Abstract

Abstract

Located in the southwest part of the Wandashan block, the Yuejinshan copper-gold deposit is a skarn type deposit, and its orebodies are hosted in skarns, granite porphyries and the tectonic fractures. The orebodies show lenticular or veined forms. LA-ICP-MS zircon U-Pb dating and geochemical data are reported for granite porphyries and granodiorites in the Yuejinshan coppergold deposit in order to constrain its formation time, petrogenesis and the minerogenetic geotectonic background. The zircon LAICP-MS U-Pb age dating results show that the petrogenic ages of granite porphyries and granodiorites respectively are(115.8±1.0) Ma and(126.9 ±1.7)Ma respectively, and the copper-gold mineralization age is consistent with petrogenetic age of granite porphyry. Geochemical study indicates that the granodiorites are peraluminous calc-alkaline granite. The chondrite-normalized REE patterns of granodiorites display LREE enrichment and HREE depletion, with a distinct Eu anomaly, and their magma came from the lower crust. The granite porphyries belong to peraluminous calc-alkaline granite. The REE patterns show that granite porphyries exhibit pronounced LREE enrichment and HREE depletion, enrichment of large-ion lithosphile elements (Rb, Ba, K, Sr) and incompatible elements (U, Th), and depletion of high field-strength elements (Ta, Nb, P, Ti) and HREE. The magma of granite porphyries came from crust-mantle mixture, and the copper-gold deposit formed in the collision of post-collision extensional tectonic setting. The metallogenic materials formed intermediate-acid magma heat source, and magmatism and mineralization took place in the extensional tectonics after the Pacific plate subduction.
- geological features,
- geochemical characteristics,
- zircon U-Pb age,
- sharn,
- Yuejinshan copper-gold deposit,
- Heilongjiang Province

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References (82)

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Zircon U-Pb age, geochemistry and genesis of acid intrusive rocks in the Yuejinshan skarn type copper-gold deposit, Wandashan block