钦杭成矿带大瑶山地区晚白垩世斑岩型铜矿床: 锆石U-Pb定年及Hf同位素制约

毕诗健; 杨振; 李巍; 梁培; 唐克非

doi:10.3799/dqkx.2015.132

Volume 40 Issue 9

Sep. 2015

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Article Navigation > Earth Science > 2015 > 40(9): 1458-1479

Bi Shijian, Yang Zhen, Li Wei, Liang Pei, Tang Kefei, 2015. Discovery of Late Cretaceous Baoshan Porphyry Copper Deposit in Dayaoshan, Qinhang Metallogenic Belt: Constraints from Zircon U-Pb Age and Hf Isotope. Earth Science, 40(9): 1458-1479. doi: 10.3799/dqkx.2015.132

Citation:

Bi Shijian, Yang Zhen, Li Wei, Liang Pei, Tang Kefei, 2015. Discovery of Late Cretaceous Baoshan Porphyry Copper Deposit in Dayaoshan, Qinhang Metallogenic Belt: Constraints from Zircon U-Pb Age and Hf Isotope. Earth Science, 40(9): 1458-1479. doi: 10.3799/dqkx.2015.132

Citation:

Bi Shijian, Yang Zhen, Li Wei, Liang Pei, Tang Kefei, 2015. Discovery of Late Cretaceous Baoshan Porphyry Copper Deposit in Dayaoshan, Qinhang Metallogenic Belt: Constraints from Zircon U-Pb Age and Hf Isotope. Earth Science, 40(9): 1458-1479. doi: 10.3799/dqkx.2015.132

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Discovery of Late Cretaceous Baoshan Porphyry Copper Deposit in Dayaoshan, Qinhang Metallogenic Belt: Constraints from Zircon U-Pb Age and Hf Isotope

doi: 10.3799/dqkx.2015.132

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Geophysical Exploration Institute of Guangxi, Liuzhou 545005, China
3.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
4.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610051, China

Received Date: 2015-05-02
Publish Date: 2015-09-15

Abstract

Abstract

The Qinzhou Bay-Hangzhou Bay suture zone is an important porphyry copper metallogenic belt in southern China. Previous studies suggest that the ages of regional diagenesis and mineralization are mainly concentrated in the Late-Middle Jurassic (180-155 Ma), and the ore-bearing granite porphyry shows distinctly crust-mantle contamination. The Baoshan copper deposit is a porphyry-type Cu deposit newly discovered in the Dayaoshan region in the southwestern of the Qinhang metallogenic belt in recent years. The granite porphyry is dominated as small stock into Sheshan granodiorite, including two outcropped and one concealed magmatic emplacement. And the copper ore body is all hosted in the Baoshan concealed granite porphyry. In this paper, laser ablation (MC)-ICPMS U-Pb dating and Hf isotopic compositions of zircons from three granite porphyry samples in the Baoshan copper deposit are presented. Highly precise U-Pb results indicate that zircons from one concealed and two outcropped granite porphyries give weighted mean ²⁰⁶Pb/²³⁸U age of 91.1±0.6 Ma (1σ), 91.3±0.8 Ma (1σ) and 90.1±1.0 Ma (1σ), respectively. And the zircons crystallized in the late Yanshannian granites give ε_Hf (91 Ma) values ranging from -8.74 to -5.13 and Hf model ages (T_DM2) of 1 210-1 394 Ma. U-Pb and Hf isotopic data can be interpreted as the crystallization time of these granites and the mineralization age, indicating it was formed in the ~91 Ma and may be developed by reworking of Mesoproterozoic crust closely related to partial melting. Together with other published geochronological data, it is proposed that the late Yanshannian magmatite and related Cu (Au)-W-Mo deposit are widely developed in the Dayaoshan and its adjacent areas. Moreover, two epochs of porphyry copper mineralization are confirmed in this study, including the Middle-Late Jurassic and the Late Cretaceous, in the Qinhang metallogenic belt, and it is concluded that Late Cretaceous mineralization possibly resulted from the post-collisional crustal extension setting in the continental margin of the South China.
- Qinzhou Bay-Hangzhou Bay metallogenic belt,
- Dayaoshan,
- Baoshan copper deposit,
- granite porphyry,
- Late Cretaceous mineralization,
- geochemistry

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References(131)

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