海南岛晨星早石炭世高度亏损N-MORB型玄武岩及其地质意义

何慧莹; 王岳军; 张玉芝; 陈新跃; 周永智

doi:10.3799/dqkx.2016.108

Volume 41 Issue 8

Aug. 2016

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Article Navigation > Earth Science > 2016 > 41(8): 1361-1375

He Huiying, Wang Yuejun, Zhang Yuzhi, Chen Xinyue, Zhou Yongzhi, 2016. Extremely Depleted Carbonferous N-MORB Metabasite at the Chenxing Area (Hainan) and Its Geological Significance. Earth Science, 41(8): 1361-1375. doi: 10.3799/dqkx.2016.108

Citation:

He Huiying, Wang Yuejun, Zhang Yuzhi, Chen Xinyue, Zhou Yongzhi, 2016. Extremely Depleted Carbonferous N-MORB Metabasite at the Chenxing Area (Hainan) and Its Geological Significance. Earth Science, 41(8): 1361-1375. doi: 10.3799/dqkx.2016.108

Citation:

He Huiying, Wang Yuejun, Zhang Yuzhi, Chen Xinyue, Zhou Yongzhi, 2016. Extremely Depleted Carbonferous N-MORB Metabasite at the Chenxing Area (Hainan) and Its Geological Significance. Earth Science, 41(8): 1361-1375. doi: 10.3799/dqkx.2016.108

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Extremely Depleted Carbonferous N-MORB Metabasite at the Chenxing Area (Hainan) and Its Geological Significance

doi: 10.3799/dqkx.2016.108

He Huiying^{1,2
,},
Wang Yuejun^{1,2
,
,},
Zhang Yuzhi^1,2,
Chen Xinyue³,
Zhou Yongzhi^1,2

1.
School of Earth Sciences and Geological Engineering, Sun Yat-Sen University, Guangzhou 510275, China
2.
Guangdong Provincial Key Laboratoroy of Mineral Resources & Geological Processes, Guangzhou 510275, China
3.
Department of Geology, Hunan University of Science and Technology, Xiangtan 411201, China

Received Date: 2016-02-06
Publish Date: 2016-08-15

Abstract

Abstract

Hainan Island, located between the Indochina and South China Blocks, has undergone compound structural overprinting and complex tectonic evolution. However, the Late Paleozoic tectonic regime and amalgamation history of the South China with Indochina Blocks are still on debate. Our investigation identified the highly-depleted greenschist-facies basalt at the Chenxing area in the north of the Changjiang-Qionghai fault, Central Hainan Island. This paper presents a set of new geochronological and geochemical data for these metabasites. The representative sample for Chenxing metabasites gave the plateau age of 328.1±2.6 Ma, representing the eruption age. They have SiO₂ ranging from 46.92 % to 52.58 %, TiO₂ from 0.48 % to 1.12% and Al₂O₃ from 12.34 % to 17.45 %, and could be classified as basalt. These samples show lower K₂O contents, and HFSEs and REEs contents relative to N-MORB. They are characterized by the left-sloping REE pattern and multi-elemental pattern with a geochemical affinity to N-MORB. These samples show extremely high ε_Nd(t) values ranging from 9.02 to 9.85. Such geochemical characteristics for the Chenxing metabasites show the derivation of the MORB source modified by slab-related fluid. In combination with other available data, the Chenxing metabasites in Central Hainan are formed in the back-arc basin or a restricted ocean basin between the South China and Indochina blocks during the Carboniferous in response to the subduction of the Paleotethyan main ocean.
- metabasites,
- Nd isotopic composition,
- N-MORB,
- Carbonferous,
- eastern paleotethyan evolution,
- geochemistry,
- petrology

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References(114)

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Extremely Depleted Carbonferous N-MORB Metabasite at the Chenxing Area (Hainan) and Its Geological Significance

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