福建平和矾山地区花岗岩地球化学、年代学、Hf同位素特征及地质意义

王森; 张达; 赵红松; 潘天望; 吕良冀; 冯海滨; 狄永军

doi:10.3799/dqkx.2016.005

Volume 41 Issue 1

Jan. 2016

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Article Navigation > Earth Science > 2016 > 41(1): 67-83

Wang Sen, Zhang Da, Zhao Hongsong, Pan Tianwang, Lü Liangji, Feng Haibin, Di Yongjun, 2016. Geochemistry, Zircon U-Pb Dating and Hf Isotope Composition of Granite in Fanshan Area, Pinghe County, Fujian Province, and Its Geological Significance. Earth Science, 41(1): 67-83. doi: 10.3799/dqkx.2016.005

Citation:

Wang Sen, Zhang Da, Zhao Hongsong, Pan Tianwang, Lü Liangji, Feng Haibin, Di Yongjun, 2016. Geochemistry, Zircon U-Pb Dating and Hf Isotope Composition of Granite in Fanshan Area, Pinghe County, Fujian Province, and Its Geological Significance. Earth Science, 41(1): 67-83. doi: 10.3799/dqkx.2016.005

Citation:

Wang Sen, Zhang Da, Zhao Hongsong, Pan Tianwang, Lü Liangji, Feng Haibin, Di Yongjun, 2016. Geochemistry, Zircon U-Pb Dating and Hf Isotope Composition of Granite in Fanshan Area, Pinghe County, Fujian Province, and Its Geological Significance. Earth Science, 41(1): 67-83. doi: 10.3799/dqkx.2016.005

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Geochemistry, Zircon U-Pb Dating and Hf Isotope Composition of Granite in Fanshan Area, Pinghe County, Fujian Province, and Its Geological Significance

doi: 10.3799/dqkx.2016.005

State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2015-09-30
Publish Date: 2016-01-15

Abstract

Abstract

In order to study the chronological and geochemical characteristics of the Mesozoic granite and granodiorite from Fanshan area and their relationship with the regional mineralization, the LA-MC-ICPMS zircons U-Pb dating method was employed to assess the ages and Hf isotope composition, preceded by their petrological and geochemical studies. In addition, the authors aim to provide more evidences that will facilitate the next phase of prospecting by making a comparison with Zijinshan copper-gold ore field. The metaluminous-peraluminous high-K calcalkaline granite series and granodiorite are characterized by high contents of K₂O, SiO₂, and low TiO₂. These samples are enriched in light rare earth element (LREE) and large ionic lithophile elements (LILE, e.g. K, Rb, Sr, Cs), but depleted in high strength elements (HFSE, e.g. Nb, Ta, Zr, Ti), and have negative Eu anomalies. The geochemical properties of granite and granodiorite are similar to those of the magmatic arc rocks, which suggest a backarc spreading setting. The zircon U-Pb dating of two representative samples yield an emplaced age of 110 Ma, in Early Cretaceous. Zircon grains from the granites have lower Hf-isotpe compositions with ε_Hf(t)=-3.1-1.6 and younger Hf model ages (T_DM2)=1 066-1 366 Ma. In comparison with the metamorphic basement near the study area, we suggest that the granitic rocks are probably derived from a Mesoproterozoic crust, but the granodiorite may have originated from a Mesoproterozoic crust-mixed with a fraction of mantle materials. Based on the comparative study with Zijinishan Orefield, it is concluded that there are similar structural, lithogeneous and metallogenic features between the two areas, and there is huge prospecting potential to find "Zijinshan style" copper-gold polymetallic deposits in Fanshan area.
- Fanshan,
- zircon U-Pb dating,
- Hf isotope,
- Zijinshan,
- petrology

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Geochemistry, Zircon U-Pb Dating and Hf Isotope Composition of Granite in Fanshan Area, Pinghe County, Fujian Province, and Its Geological Significance

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