阿拉善北部亚干地区花岗岩锆石年代学、地球化学特征及其构造意义

史兴俊; 张磊; 张辰光; 张建军; 丁自源; 张勇; 包峻帆; 周红升

doi:10.3799/dqkx.2020.164

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2469-2484

Shi Xingjun, Zhang Lei, Zhang Chenguang, Zhang Jianjun, Ding Ziyuan, Zhang Yong, Bao Junfan, Zhou Hongsheng, 2020. Zircon Geochronology and Geochemistry of the Granitoids in Yagan Area, Northern Alxa and Their Tectonic Implications. Earth Science, 45(7): 2469-2484. doi: 10.3799/dqkx.2020.164

Citation:

Shi Xingjun, Zhang Lei, Zhang Chenguang, Zhang Jianjun, Ding Ziyuan, Zhang Yong, Bao Junfan, Zhou Hongsheng, 2020. Zircon Geochronology and Geochemistry of the Granitoids in Yagan Area, Northern Alxa and Their Tectonic Implications. Earth Science, 45(7): 2469-2484. doi: 10.3799/dqkx.2020.164

Citation:

Shi Xingjun, Zhang Lei, Zhang Chenguang, Zhang Jianjun, Ding Ziyuan, Zhang Yong, Bao Junfan, Zhou Hongsheng, 2020. Zircon Geochronology and Geochemistry of the Granitoids in Yagan Area, Northern Alxa and Their Tectonic Implications. Earth Science, 45(7): 2469-2484. doi: 10.3799/dqkx.2020.164

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Zircon Geochronology and Geochemistry of the Granitoids in Yagan Area, Northern Alxa and Their Tectonic Implications

doi: 10.3799/dqkx.2020.164

1.
College of Geographic Sciences, Xinyang Normal University, Xinyang 464000, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
No.3 Institute of Geological and Mineral Resources Survey, Henan Bureau of Geoexploration and Mineral Development, Xinyang 464000, China

Received Date: 2020-06-20
Publish Date: 2020-07-15

Abstract

Abstract

Due to the lack of detailed field geological and high-precision geochronological studies, the basement nature and tectonic attribute of the Yagan area have been poorly understood so far, which prevent the further understanding of the basic architecture and tectonic evolution of the southern Central Asian orogenic belt. Revealing the age and origin of the granitoids is essential for the understanding of the basement characteristics and tectonic architecture. In this paper presents systematic petrology, zircon U-Pb and Hf isotopic studies for the granitoids in the Yagan area.LA-ICP-MS zircon U-Pb isotopic dating results indicate that the biotite-monzonitic granite of Qiedao pluton and granodiorite of Yadong pluton emplaced at 380±1 Ma and 271±2 Ma, respectively. Meanwhile, the zircon U-Pb ages of 228±2 Ma and 214±2 Ma were obtained from the gneissic granite and mylonitic granite (their protoliths are granite rocks) in Paleoproterozic Beishan Group. Mineralogical and geochemical features suggest that the Qiedao and Dure granites are high-K calc-alkaline and metaluminous to slightly peraluminous, belonging to the A-type granites, and the Yadong granodiorites are calc-alkaline I-type granites. The Qiedao biotite-monzonitic granite and Yadong granodiorite have zircon ε_Hf(t) values ranging from -2.8 to +4.3 and the crustal model ages of 1.5 to 1.0 Ga, suggesting that the magma sources were mainly derived from the Meso-proterozoic crustal material.Inherited zircon ages within the gneissic granite are mainly around 0.8-1.0 Ga. These observations, in combination with previous work, indicate that the basement of Yagan area is composed of Meso-Neoproterozoic rocks, and the South Gobi microcontinent might extend into the northern Alxa.
- Yagan,
- south Gobi microcontinent,
- granitoid,
- zircon Hf isotope,
- Central Asian orogenic belt,
- geochemistry

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References(120)

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