粤南海宴A型花岗岩与镁铁质包体的成因及意义

贾小辉; 谢国刚; 孟德磊; 万乐; 吴俊; 卜建军; 吴富强; 曾海良; 卢加文; 詹瑞华

doi:10.3799/dqkx.2018.184

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2294-2309

Jia Xiaohui, Xie Guogang, Meng Delei, Wan Le, Wu Jun, Bu Jianjun, Wu Fuqiang, Zeng Hailiang, Lu Jiawen, Zhan Ruihua, 2018. Petrogenesis and Implications of the Haiyan A-Type Granites and Mafic Microgranule Enclaves in Southern Guangdong Province. Earth Science, 43(7): 2294-2309. doi: 10.3799/dqkx.2018.184

Citation:

Jia Xiaohui, Xie Guogang, Meng Delei, Wan Le, Wu Jun, Bu Jianjun, Wu Fuqiang, Zeng Hailiang, Lu Jiawen, Zhan Ruihua, 2018. Petrogenesis and Implications of the Haiyan A-Type Granites and Mafic Microgranule Enclaves in Southern Guangdong Province. Earth Science, 43(7): 2294-2309. doi: 10.3799/dqkx.2018.184

Citation:

Jia Xiaohui, Xie Guogang, Meng Delei, Wan Le, Wu Jun, Bu Jianjun, Wu Fuqiang, Zeng Hailiang, Lu Jiawen, Zhan Ruihua, 2018. Petrogenesis and Implications of the Haiyan A-Type Granites and Mafic Microgranule Enclaves in Southern Guangdong Province. Earth Science, 43(7): 2294-2309. doi: 10.3799/dqkx.2018.184

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Petrogenesis and Implications of the Haiyan A-Type Granites and Mafic Microgranule Enclaves in Southern Guangdong Province

doi: 10.3799/dqkx.2018.184

1.
Wuhan Center of China Geological Survey, Wuhan 430223, China
2.
Research Center for Petrogenesis and Mineralization of Granitoid Rocks, China Geological Survey, Wuhan 430223, China
3.
No. 912 Geological Surveying Party, Jiangxi Bureau of Geology and Mineral Exploration and Development, Yingtan 335001, China

Received Date: 2017-11-23
Publish Date: 2018-07-15

Abstract

Abstract

The study of the late Mesozoic granites in South China and its tectonic setting is a hotspot issue. In this paper, new zircon U-Pb ages and geochemical data of the Haiyan A-type granites and mafic microgranule enclaves (MMEs) in southern Guangdong are reported, and the petrogenesis and implications of these rocks are discussed. We present new zircon LA-ICP-MS U-Pb ages of the Haiyan granites and its MMEs, and the results of the age analyzing show that the granites and MMEs were generated in Early Cretaceous (144.0±1.7 Ma and 141.1±2.5 Ma, respectively). The Haiyan granites have the typical features of A-type granites, they are characterized by enrichment in silicon, alkali and iron contents, and depletion in magnesium and calcium contents, with high 10 000×Ga/A1 values and Zr+Nb+Ce+Y components. Small amounts of MMEs occur in the Haiyan granites, and they are characterized by enrichment in alkali and more enrichment in potassium contents, high aluminum and low titanium, strong enrichment in the large ion lithophile elements and light rare earth elements, belonging to shoshonitic rocks. Granites have I_Sr values of 0.706 6-0.712 2, ε_Nd(t) values of -7.01——2.03. While MMES have relatively lower I_Sr values (0.708 5-0.711 1) and higher ε_Nd(t) values (-6.99——2.23). Combining with geochemical and Sr-Nd isotopic compositions, we suggest that the Haiyan granites were likely generated by partial melting of the Mesoproterozoic crustal rocks, and the primitive compositions of shoshonitic MMEs likely originated from enriched mantle source somatized by subducted oceanic sediments. The findings of the Haiyan A-type granites and shoshonitic mafic enclaves suggest that the regional tectonic setting during the Early Cretaceous was in extension, and different from southeast coastal areas with compressive tectonic regime.
- Early Cretaceous,
- A-type granite,
- shoshonitic rocks,
- extension,
- South China,
- geochronology

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References(90)

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Petrogenesis and Implications of the Haiyan A-Type Granites and Mafic Microgranule Enclaves in Southern Guangdong Province

doi: 10.3799/dqkx.2018.184

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