越南昆嵩地体三叠纪花岗岩岩石成因及其特提斯构造意义

李慧玲; 钱鑫; 余小清; PhamTrungHieu; 张菲菲; 余永琪; 徐畅; 王岳军

doi:10.3799/dqkx.2022.335

Volume 48 Issue 4

Apr. 2023

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Article Navigation > Earth Science > 2023 > 48(4): 1441-1460

Li Huiling, Qian Xin, Yu Xiaoqing, Pham Trung Hieu, Zhang Feifei, Yu Yongqi, Xu Chang, Wang Yuejun, 2023. Petrogenesis of Triassic Granites from Kontum Massif in Vietnam and Its Tethyan Tectonic Implications. Earth Science, 48(4): 1441-1460. doi: 10.3799/dqkx.2022.335

Citation:

Li Huiling, Qian Xin, Yu Xiaoqing, Pham Trung Hieu, Zhang Feifei, Yu Yongqi, Xu Chang, Wang Yuejun, 2023. Petrogenesis of Triassic Granites from Kontum Massif in Vietnam and Its Tethyan Tectonic Implications. Earth Science, 48(4): 1441-1460. doi: 10.3799/dqkx.2022.335

Citation:

Li Huiling, Qian Xin, Yu Xiaoqing, Pham Trung Hieu, Zhang Feifei, Yu Yongqi, Xu Chang, Wang Yuejun, 2023. Petrogenesis of Triassic Granites from Kontum Massif in Vietnam and Its Tethyan Tectonic Implications. Earth Science, 48(4): 1441-1460. doi: 10.3799/dqkx.2022.335

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Petrogenesis of Triassic Granites from Kontum Massif in Vietnam and Its Tethyan Tectonic Implications

doi: 10.3799/dqkx.2022.335

Li Huiling^{1
,
,},
Qian Xin^{1, 2
,
,
,},
Yu Xiaoqing¹,
Pham Trung Hieu³,
Zhang Feifei⁴,
Yu Yongqi¹,
Xu Chang¹,
Wang Yuejun^{1, 2}

1.
Guangdong Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Zhuhai 519082, China
2.
Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai 519082, China
3.
Faculty of Geology, Vietnam National University, Ho Chi Minh 70000, Vietnam
4.
Department of Geology, Northwest University, Xi'an 710069, China

Received Date: 2022-07-12
Publish Date: 2023-04-25

Abstract

Abstract

Kontum massif in the central Indochina records abundant Indosinian magmatism and tectonic thermal events, and is a key area for investigating the tectonic evolution of Paleotethyan ocean and subsequent collision between the Indochina and South China blocks. However, the origin of this Indosinian magmatism and its relationship with the Truong Son zone in the north are poorly constrained. In this study, it presents a set of petrographic, zircon U-Pb geochronological, zircon in-situ Hf isotopic, and whole-rock geochemical data for the granites from the Huyen Tuy An and Chu Loan area in the Kontum massif to constrain their crystallization ages, petrogenesis, and tectonic setting. Zircon U-Pb dating shows that the granites formed at 244-239 Ma. These samples contain monzogranites and K-feldspar granites and belong to the high-K calc-alkaline series. They are S-type granites with A/CNK values ranging from 1.03 to 1.21. These samples show enrichment of Rb, Th, and U, and depletion of Nb, Sr, Zr, and Ti, with obvious negative Eu anomalies (Eu/Eu*=0.24-0.56). Their negative zircon ε_Hf(t) values ((-11.2)-(-0.7)) and Paleo- to Meso-Proterozoic Hf model ages (T_DM2=1.98-1.31 Ga) indicate that these granites were derived from the partial melting of the Paleo- to Meso-Proterozoic metasedimentary rocks with a small amount of metaigneous component. Our new data along with the regional geological observations suggest that the Middle Triassic Van Canh granites in the Kontum massif were formed in a post-collisional setting in response to the collision between the Indochina and South China blocks following the closure of Song-Ma Paleotethyan branch. Our studies further suggest that the Truong Son zone can southerly extend to the central Kontum massif.
- Indochina block,
- Kontum massif,
- Middle Triassic,
- S-type granite,
- Paleotethyan ocean,
- post-collision,
- geochemistry

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References(141)

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Petrogenesis of Triassic Granites from Kontum Massif in Vietnam and Its Tethyan Tectonic Implications

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