豫南新县岩体地球化学、年代学和Hf同位素特征及地质意义

刘清泉; 邵拥军; 陈昕梦; 刘忠法; 张喆

doi:10.3799/dqkx.2016.507

Volume 41 Issue 8

Aug. 2016

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Article Navigation > Earth Science > 2016 > 41(8): 1275-1294

Liu Qingquan, Shao Yongjun, Chen Xinmeng, Liu Zhongfa, Zhang Zhe, 2016. Petrogeochemistry, Geochronology and Hf Isotopes of the Monzogranite from Xinxian, Southern Region in Henan Province. Earth Science, 41(8): 1275-1294. doi: 10.3799/dqkx.2016.507

Citation:

Liu Qingquan, Shao Yongjun, Chen Xinmeng, Liu Zhongfa, Zhang Zhe, 2016. Petrogeochemistry, Geochronology and Hf Isotopes of the Monzogranite from Xinxian, Southern Region in Henan Province. Earth Science, 41(8): 1275-1294. doi: 10.3799/dqkx.2016.507

Citation:

Liu Qingquan, Shao Yongjun, Chen Xinmeng, Liu Zhongfa, Zhang Zhe, 2016. Petrogeochemistry, Geochronology and Hf Isotopes of the Monzogranite from Xinxian, Southern Region in Henan Province. Earth Science, 41(8): 1275-1294. doi: 10.3799/dqkx.2016.507

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Petrogeochemistry, Geochronology and Hf Isotopes of the Monzogranite from Xinxian, Southern Region in Henan Province

doi: 10.3799/dqkx.2016.507

Liu Qingquan^{1,2,3
,},
Shao Yongjun^{1,2
,
,},
Chen Xinmeng⁴,
Liu Zhongfa^1,2,
Zhang Zhe³

1.
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083, China
2.
School of Geosciences and Info-Physics, Central South University, Changsha 410083, China
3.
Henan Nonferrous Metals Geological Exploration Institute, Zhengzhou 450052, China
4.
The Seventh Geological Brigade of Henan Nonferrous Metals Geological Mineral Resources Bureau, Zhengzhou 450016, China

Received Date: 2015-03-28
Publish Date: 2016-08-15

Abstract

Abstract

Xinxian monzogranites are located at the Qinling-Dabie orogenic belt, and a systematic geochemical study can facilitate further studies on the Mesozoic tectono-magmatic evolution and the geodynamics background of Qinling-Dabie orogenic belt. This paper presents geochemistry, zircon U-Pb geochronology, and Hf-isotopic data of the rocks, with the aim of constraining their petrogenesis, sources and tectonic implications. The geochemical analysis shows that Xinxian monzogranites are characterized by SiO₂=74.94%-78.16%, K₂O=3.87%-5.86%, Na₂O=3.82%-4.24%, Al₂O₃=12.38%-13.57%, A/CNK=1.05-1.11; the rocks are enriched in LREE, depleted HREE and negative Eu anomalies, enriched in Rb, U, Hf, Y and depleted Ba, Nb, Ta, Ti, which indicates that Xinxian monzogranites are peraluminous, high-K calc-alkaline Ⅰ-type granite. The three stages yield LA-ICP-MS zircon U-Pb ages 153.4±1.1 Ma, 146.4±1.6 Ma and 131.6±1.8 Ma respectively. According to zircon Hf isotope analysis, the ε_Hf(t) values of the granite range from -24.5 to -20.3, which locates below the depleted mantle line. The t_DM2 values range from 2.68 to 2.93 Ga, which indicates the monzogranites resulted from the lower crust of Yangtze Block. The component of the monzogranite is similar to that of Neoproterozoic TTG magmatic rocks. Xinxian monzogranites were emplaced after the major collisional period of the North China block and Yangtze block, in the post-collisional tectonic setting under the regional extension mechanism. The geodynamics setting is the transformation of tectonic regime of the Late Jurassic-Early Cretaceous and large-scale lithosphere delaminating thinning under post stretching mechanism.
- Dabie mountain,
- Xinxian,
- monzogranite,
- petrology,
- geochemistry,
- geochronology,
- Hf isotope

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References(137)

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Petrogeochemistry, Geochronology and Hf Isotopes of the Monzogranite from Xinxian, Southern Region in Henan Province

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