A newly Found Biotite Syenogranite in the A newly Found Biotite Syenogranite in the Huangshaping Polymetallic Deposit, South China: Insights into Cu Mineralization

Weicheng Jiang; Huan Li; Jinghua Wu; Zhekai Zhou; Hua Kong; Jingya Cao

doi:10.1007/s12583-017-0974-7

Volume 29 Issue 3

Aug 2018

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Journal of Earth Science > 2018 > 29(3): 537-555.

Weicheng Jiang, Huan Li, Jinghua Wu, Zhekai Zhou, Hua Kong, Jingya Cao. A newly Found Biotite Syenogranite in the A newly Found Biotite Syenogranite in the Huangshaping Polymetallic Deposit, South China: Insights into Cu Mineralization. Journal of Earth Science, 2018, 29(3): 537-555. doi: 10.1007/s12583-017-0974-7

Citation:

Weicheng Jiang, Huan Li, Jinghua Wu, Zhekai Zhou, Hua Kong, Jingya Cao. A newly Found Biotite Syenogranite in the A newly Found Biotite Syenogranite in the Huangshaping Polymetallic Deposit, South China: Insights into Cu Mineralization. Journal of Earth Science, 2018, 29(3): 537-555. doi: 10.1007/s12583-017-0974-7

Citation:

Weicheng Jiang, Huan Li, Jinghua Wu, Zhekai Zhou, Hua Kong, Jingya Cao. A newly Found Biotite Syenogranite in the A newly Found Biotite Syenogranite in the Huangshaping Polymetallic Deposit, South China: Insights into Cu Mineralization. Journal of Earth Science, 2018, 29(3): 537-555. doi: 10.1007/s12583-017-0974-7

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A newly Found Biotite Syenogranite in the A newly Found Biotite Syenogranite in the Huangshaping Polymetallic Deposit, South China: Insights into Cu Mineralization

doi: 10.1007/s12583-017-0974-7

1.
Faculty of Earth Resources, State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha 410083, China
3.
CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China

More Information

Corresponding author: Huan Li, lihuan@csu.edu.cn
Received Date: 30 Jul 2017
Accepted Date: 20 Dec 2017
Publish Date: 01 Jun 2018

Abstract

Abstract

The W-Sn-Mo-Cu-Pb-Zn polymetallic mineralization in the Huangshaping Deposit is associated with different types of Jurassic granitic intrusions such as quartz porphyry, granophyre and granite porphyry. In this study, we carried out detailed mineralogical, petrological, geochemical, zircon U-Pb geochronological and Hf isotopic studies on a newly found, Cu-mineralization-related fine- grained biotite syenogranite at Huangshaping. This syenogranite is mainly composed of quartz (40%), K-feldspar (30%), plagioclase (15%) and biotite (5%), enriching in SiO₂ (75.58 wt.%-76.02 wt.%), K₂O (5.24 wt.%-5.78 wt.%), Al₂O₃ (12.23 wt.%-12.46 wt.%), Rb (405 ppm-504 ppm), U (18.5 ppm-40.7 ppm), Th (47 ppm-52.3 ppm), Nb (49.6 ppm-57.5 ppm), and Cu (54 ppm-288 ppm) whereas depleting in P₂O₅ (0.01 wt.%), TiO₂ (0.05 wt.%-0.06 wt.%), Ba (5 ppm-13.1 ppm), Sr (6.8 ppm-23.9 ppm) and Eu (0.04 ppm-0.05 ppm), with A₁-type alkaline granite characteristics. Magmatic and hydrothermal zircons were separated from a Cu-mineralized syenogranite sample and yielded the ²⁰⁶Pb/²³⁸U concordant ages of 156.5±1.8 and 154.4±2.9 Ma, representing the intrusive age of the pluton and probable Cu-mineralization time at the Huangshaping Deposit, respectively. Zircon Hf isotopes suggest a crust-derived (partial melting of Paleoproterozoic basement) magma for the syenogranite, with some degree of crust-mantle interaction. We infer that the syenogranite is a transitional phase between the granophyre and the granite porphyry, not only contributed greatly to the Cu mineralization but also provided W-Sn polymetallic ore-forming metals for the Huangshaping Deposit.
- zircon U-Pb dating,
- Hf isotope,
- A-type granite,
- southern Hunan

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References(90)

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