苏门答腊岛北部Takengon早志留世S型花岗片麻岩年代学、地球化学特征及构造意义

徐畅; 王岳军; 钱鑫; 张玉芝; 余小清

doi:10.3799/dqkx.2020.030

Volume 45 Issue 6

Jun. 2020

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Xu Chang, Wang Yuejun, Qian Xin, Zhang Yuzhi, Yu Xiaoqing, 2020. Geochronological and Geochemical Characteristics of Early Silurian S-Type Granitic Gneiss in Takengon Area of Northern Sumatra and Its Tectonic Implications. Earth Science, 45(6): 2077-2090. doi: 10.3799/dqkx.2020.030

Citation:

Xu Chang, Wang Yuejun, Qian Xin, Zhang Yuzhi, Yu Xiaoqing, 2020. Geochronological and Geochemical Characteristics of Early Silurian S-Type Granitic Gneiss in Takengon Area of Northern Sumatra and Its Tectonic Implications. Earth Science, 45(6): 2077-2090. doi: 10.3799/dqkx.2020.030

Citation:

Xu Chang, Wang Yuejun, Qian Xin, Zhang Yuzhi, Yu Xiaoqing, 2020. Geochronological and Geochemical Characteristics of Early Silurian S-Type Granitic Gneiss in Takengon Area of Northern Sumatra and Its Tectonic Implications. Earth Science, 45(6): 2077-2090. doi: 10.3799/dqkx.2020.030

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Geochronological and Geochemical Characteristics of Early Silurian S-Type Granitic Gneiss in Takengon Area of Northern Sumatra and Its Tectonic Implications

doi: 10.3799/dqkx.2020.030

Xu Chang^{1, 2
,
,},
Wang Yuejun^{1, 2},
Qian Xin^{1, 2
,
,},
Zhang Yuzhi^{1, 2},
Yu Xiaoqing^{1, 2}

1.
Guangdong Provincial Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou 510275, China
2.
Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai), Zhuhai 519000, China

Received Date: 2019-12-21
Publish Date: 2020-06-15

Abstract

Abstract

Sumatra Island is located in the southwestern margin of the Sundaland, and is divided into East/West Sumatra by the Medial Sumatran Zone. While East Sumatran basement affinity and tectonic evolution are not well defined. The Early Paleozoic granitic gneisses have been identified from the East Sumatra Terrane, with providing zircon U-Pb age, in-situ Hf isotopic and geochemical results. Geochronological result yields a ²⁰⁶Pb/²³⁸U mean age of 442 ±5 Ma (MSWD = 1.03), representing the crystalline age. Zircon ε_Hf (t) values range from -1.3 to -7.8. The whole-rock geochemical characteristics show that our samples are characterized by high SiO₂ (69.97%-74.30%) and Al₂O₃ (13.90%-15.93%), but poor in TiO₂ (0.48%-0.61%), MgO (0.54%-0.93%) and CaO (0.11%-0.25%). These samples have high A/CNK (2.58-3.06) and CIPW-normalized corundum (10.0%-11.4%), similar to those of the S-type granite. They have obvious fractionation between LREEs and HREEs. These samples are characterized by enrichment in LILEs (Rb, Th, U) and depletion in HFSEs (Nb, Ta, Ti). The geochemical results indicate that the Takengon granitic gneisses are originated from the partial melting of the meta-sediments during the evolution of the Prototethyan Ocean. This study confirms the existing of Early Silurian basement rocks in the East Sumatra Terrane, which were related to the Prototethyan evolution.
- granitic gneiss,
- Early Silurian,
- Sumatra,
- prototethyan,
- zircon U-Pb geochronology,
- zircon Hf isotopes,
- geochemistry

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References(76)

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