海南荔枝沟中三叠世酸性火山岩年代学、地球化学特征及其构造意义

芶琪钰; 钱鑫; 何慧莹; 张玉芝; 王岳军

doi:10.3799/dqkx.2018.161

Volume 44 Issue 4

Apr. 2019

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Gou Qiyu, Qian Xin, He Huiying, Zhang Yuzhi, Wang Yuejun, 2019. Geochronological and Geochemical Constraints on Lizhigou Middle Triassic Felsic Volcanic Rocks in Hainan and Its Tectonic Implications. Earth Science, 44(4): 1357-1370. doi: 10.3799/dqkx.2018.161

Citation:

Gou Qiyu, Qian Xin, He Huiying, Zhang Yuzhi, Wang Yuejun, 2019. Geochronological and Geochemical Constraints on Lizhigou Middle Triassic Felsic Volcanic Rocks in Hainan and Its Tectonic Implications. Earth Science, 44(4): 1357-1370. doi: 10.3799/dqkx.2018.161

Citation:

Gou Qiyu, Qian Xin, He Huiying, Zhang Yuzhi, Wang Yuejun, 2019. Geochronological and Geochemical Constraints on Lizhigou Middle Triassic Felsic Volcanic Rocks in Hainan and Its Tectonic Implications. Earth Science, 44(4): 1357-1370. doi: 10.3799/dqkx.2018.161

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Geochronological and Geochemical Constraints on Lizhigou Middle Triassic Felsic Volcanic Rocks in Hainan and Its Tectonic Implications

doi: 10.3799/dqkx.2018.161

Guangdong Provincial Key Laboratory of Geodynamics and Geohazards; School of Earth Science and Engineering, Sun Yat-sen University, Guangzhou 510275, China

Received Date: 2018-04-03
Publish Date: 2019-04-15

Abstract

Abstract

Hainan Island, which is located between the Indochina and South China blocks, has undergone multiphased structural overprinting and complex tectonic evolution.However, the Late Paleozoic tectonic regime and amalgamation process of the South China with Indochina blocks are still controversial. The newly-identified felsic volcanic rocks in the Lizhigou area are important for understanding the Early Mesozoic tectonic evolution in Hainan. LA-ICP-MS zircon U-Pb dating results show that the representative rhyolite samples yield a weighted mean ²⁰⁶Pb/²³⁸U age of 241±6 Ma (MSWD=0.9). These samples contain SiO₂ ranging from 72.34% to 77.83%, Al₂O₃ from 10.51% to 13.53%, K₂O from 2.85% to 4.85% and Na₂O from 1.75% to 3.79%.The A/CNK values range from 0.99 to 2.07. These samples have REE concentrations of 87×10^-6 to 177×10^-6, and Eu/Eu^* of 0.49-0.65.They are characterized by subparallel right-sloping REE pattern and enrichment in LREEs and LILEs, and depletion in HFSEs, similar to those of arc volcanics. Their ε_Nd(t) values range from -12.1 to -11.3. These felsic volcanic rocks are the products of partial melting of metasediments with significant fractionation crystallization. In combination with other available data, it is inferred that the Lizhigou felsic volcanic rocks can be compared with the Middle-Late Triassic igneous rocks along the Jinshajiang-Ailaoshan-Songma zone, and formed during the assemblage of the South China with Indochina blocks related to East Paleotethyan consumption.
- Middle Triassic,
- felsic volcanic rock,
- geochronology,
- geochemistry,
- post-collisional setting,
- Hainan Island

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Geochronological and Geochemical Constraints on Lizhigou Middle Triassic Felsic Volcanic Rocks in Hainan and Its Tectonic Implications

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