Volume 93, Issue 4 pp. 874-900
Original Article
Full Access

Petrogenesis and Mineralization of Two-Stage A-Type Granites in Jiuyishan, South China: Constraints from Whole-rock Geochemistry, Mineral Composition and Zircon U-Pb-Hf Isotopes

Ye LIU

Ye LIU

Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083 China

School of Geosciences and Info-Physics, Central South University, Changsha 410083 China

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Jianqing LAI

Corresponding Author

Jianqing LAI

Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083 China

School of Geosciences and Info-Physics, Central South University, Changsha 410083 China

Corresponding author. E-mail: [email protected]; [email protected]Search for more papers by this author
Wenzhou XIAO

Corresponding Author

Wenzhou XIAO

Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083 China

School of Geosciences and Info-Physics, Central South University, Changsha 410083 China

Corresponding author. E-mail: [email protected]; [email protected]Search for more papers by this author
Dick JEFFREY

Dick JEFFREY

Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083 China

School of Geosciences and Info-Physics, Central South University, Changsha 410083 China

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Rijun DU

Rijun DU

Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083 China

School of Geosciences and Info-Physics, Central South University, Changsha 410083 China

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Shuanglian LI

Shuanglian LI

Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083 China

School of Geosciences and Info-Physics, Central South University, Changsha 410083 China

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Chaoyun LIU

Chaoyun LIU

Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083 China

School of Geosciences and Info-Physics, Central South University, Changsha 410083 China

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Chunhua WEN

Chunhua WEN

Hunan Institute of Geological Survey, Changsha 410116 China

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Xiaohang YU

Xiaohang YU

College of Marine Science and Technology, China University of Geosciences, Wuhan 430074 China

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First published: 07 May 2019
Citations: 13

About the first author:

LIU Ye, female, born in 1994, postgraduate student of School of Geosciences and Info-Physics, Central South University, majored in Geological Resources and Geological Engineering. Email: [email protected]

About the corresponding author:

LAI Jianqing, male, born in 1964, professor of School of Geosciences and Info-Physics, Central South University. He is interested in the study of petrology, mineral deposits and fluid inclusions. Email: [email protected]

XIAO Wenzhou, male, born in 1991, PhD student of School of Geosciences and Info-Physics, Central South University. He is interested in the study of granitoid rocks, rare metal deposits and zircons. Email: [email protected]

Abstract

The Jiuyishan complex massif, located in the northern section of the Nanling region, is a combination of five plutons, namely, the Xuehuading, Jinjiling, Pangxiemu, Shaziling and Xishan plutons. Whole-rock geochemistry, mineral electron microprobe analysis, zircon U-Pb dating and Hf isotope analysis were carried out for the Jinjiling and Pangxiemu plutons. The zircon U-Pb dating yields weighted mean ages of 152.9±0.9 Ma for the Jinjiling pluton and 151.7±1.5 Ma for the Pangxiemu pluton, with a narrow gap between them. The Jinjiling and Pangxiemu plutons both have geochemical characteristics of high SiO2, Al2O3, Na2O, K2O and low TiO2, MgO, CaO, P2O5 contents, with intense depletionS in Sr, Ba, Ti, Eu and enrichments in Ga, FeOT and HFSE, and these characteristics reflect an A-type affinity. From the Jinjiling to the Pangxiemu plutons, the mineral composition of mica changes from lepidomelane to zinnwaldite, with increases in F, Li2O and Rb2O contents. The mineral composition of zircon changes from low Zr/Hf to high Zr/Hf, with increasing HfO2, P2O5 and UO2+ThO2+Y2O3 contents. The mineral compositions of feldspar indicate that the Pangxiemu pluton contains more alkali feldspar than the Jinjiling pluton. The whole-rock geochemistry and mineral compositions reveal a higher degree of differentiation for the Pangxiemu pluton. The nearly uniform εHf(t) indicates the same source region for the two plutons: both were derived from partial melting of the lower crust, with small contributions of mantle materials. In addition, higher F, lower Nb/Ta and Zr/Hf ratios in the Pangxiemu Pluton suggest a closer relationship with the rare metal mineralization than for the Jinjiling pluton.

 

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