琼东南晚二叠世I型花岗岩成因及其构造指示

赵国锋; 刘汇川; 钱鑫; 张爱梅; 何景文; 何慧莹; 王岳军

doi:10.3799/dqkx.2018.723

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1321-1332

Zhao Guofeng, Liu Huichuan, Qian Xin, Zhang Aimei, He Jingwen, He Huiying, Wang Yuejun, 2018. Petrogenesis of Late Permian I-Type Granites in SE Hainan Island and Its Tectonic Implication for Paleotethyan Evolution. Earth Science, 43(4): 1321-1332. doi: 10.3799/dqkx.2018.723

Citation:

Zhao Guofeng, Liu Huichuan, Qian Xin, Zhang Aimei, He Jingwen, He Huiying, Wang Yuejun, 2018. Petrogenesis of Late Permian I-Type Granites in SE Hainan Island and Its Tectonic Implication for Paleotethyan Evolution. Earth Science, 43(4): 1321-1332. doi: 10.3799/dqkx.2018.723

Citation:

Zhao Guofeng, Liu Huichuan, Qian Xin, Zhang Aimei, He Jingwen, He Huiying, Wang Yuejun, 2018. Petrogenesis of Late Permian I-Type Granites in SE Hainan Island and Its Tectonic Implication for Paleotethyan Evolution. Earth Science, 43(4): 1321-1332. doi: 10.3799/dqkx.2018.723

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Petrogenesis of Late Permian I-Type Granites in SE Hainan Island and Its Tectonic Implication for Paleotethyan Evolution

doi: 10.3799/dqkx.2018.723

1.
Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275, China
2.
Third Institute of Oceanographyh, State Oceanic Administration, Xiamen 361005, China

Received Date: 2017-11-24
Publish Date: 2018-04-15

Abstract

Abstract

Hainan Island is located in the convergence zone of the Pacific and Tethys tectonic domains and is a key area for investigating the Pacific and Tethyan evolution of the Indochina and South China blocks. In this paper, a set of new zircon U-Pb and Lu-Hf isotopic data, along with whole-rock elemental and Sr-Nd isotopic analytical results for the Changzheng and Lingshui granitoid plutons in Southeast Hainan Island are presented. The Changzheng and Lingshui granodiorites yield Late Permian LA-ICP-MS zircon U-Pb ages of 251±2 Ma and 256±1 Ma, respectively. They show K₂O/Na₂O=0.2-0.9, FeO^T/MgO ratios of 0.90, A/CNK=0.74-0.96 with 0.00-0.18% corundum. Their ε_Nd(t) values range from -6.0 to -3.2 and in-situ zircon ε_Hf(t) values from -4.4 to +0.2. Such signatures, in combination with the absence of muscovite, cordierite and garnet, suggest that these Late Permian granodiorites are I-type granites. The Changzheng and Lingshui granites were derived from the subalkaline metabasites in response to the closure of the Jinshajiang-Ailaoshan-Songma-Bangxi-Chenxing branch/back-arc basin during Paleotethyan evolution.
- Hainan Island,
- Paleotethyan evolution,
- I-type granite,
- Late Permian,
- Indosinian orogeny,
- petrology

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References(56)

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