东阿拉善地块叠布斯格杂岩的形成与变质时代：来自黑云斜长片麻岩锆石LA-ICP-MS U-Pb定年的新证据

邹雷; 刘平华; 刘利双; 王伟; 田忠华

doi:10.3799/dqkx.2020.126

Volume 45 Issue 9

Sep. 2020

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Zou Lei, Liu Pinghua, Liu Lishuang, Wang Wei, Tian Zhonghua, 2020. Diagenetic and Metamorphic Timing of the Diebusige Complex, the Eastern Alxa Block: New Evidence from Zircon LA-ICP-MS U-Pb Dating of Biotite-Plagioclase Gneiss. Earth Science, 45(9): 3313-3329. doi: 10.3799/dqkx.2020.126

Citation:

Zou Lei, Liu Pinghua, Liu Lishuang, Wang Wei, Tian Zhonghua, 2020. Diagenetic and Metamorphic Timing of the Diebusige Complex, the Eastern Alxa Block: New Evidence from Zircon LA-ICP-MS U-Pb Dating of Biotite-Plagioclase Gneiss. Earth Science, 45(9): 3313-3329. doi: 10.3799/dqkx.2020.126

Citation:

Zou Lei, Liu Pinghua, Liu Lishuang, Wang Wei, Tian Zhonghua, 2020. Diagenetic and Metamorphic Timing of the Diebusige Complex, the Eastern Alxa Block: New Evidence from Zircon LA-ICP-MS U-Pb Dating of Biotite-Plagioclase Gneiss. Earth Science, 45(9): 3313-3329. doi: 10.3799/dqkx.2020.126

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Diagenetic and Metamorphic Timing of the Diebusige Complex, the Eastern Alxa Block: New Evidence from Zircon LA-ICP-MS U-Pb Dating of Biotite-Plagioclase Gneiss

doi: 10.3799/dqkx.2020.126

Zou Lei^{1, 2, 3
,
,},
Liu Pinghua^{4
,
,},
Liu Lishuang^{1, 3},
Wang Wei⁴,
Tian Zhonghua⁴

1.
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, CAS, Beijing 100029, China
2.
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100039, China
3.
Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing 100029, China
4.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2020-04-22
Publish Date: 2020-09-15

Abstract

Abstract

The Diebusige Complex, as the oldest metamorphic complex with the highest metamorphic grade from the Alxa Block, is an excellent object to investigate the formation, evolution, and tectonic affinity of the Alxa Block. This paper presents comprehensive studies on the biotite-plagioclase gneiss from the Diebusige Complex, including detailed field investigation, petrological observation and LA-ICP-MS zircon U-Pb dating. The detrital zircon U-Pb dating indicates that the ages of the detrital zircons from the biotite-plagioclase gneiss in the Diebusige Complex are between 2 177 and 2 010 Ma, with a peak age of ca. 2 050 Ma. Combined with the maximum metamorphic age of 1 969 Ma, it is proposed that the depositional timing of the biotite-plagioclase gneiss is 2 050~1 969 Ma. Comprehensive comparative analysis shows that the depositional timing and provenance of the biotite-plagioclase gneiss in the Diebusige Complex is highly consistent with the meta-sedimentary rocks from the Longshoushan Complex and the Khondalite Belt (especially the western part of the Khondalite Belt). In addition, metamorphic zircon U-Pb dating and REE analyses indicate that the metamorphic zircons of the biotite-plagioclase gneiss yield continuous ages of 1 969~1 811 Ma. Based on the similarities in the detrital zircon age patterns and metamorphic timing of the meta-sedimentary rocks from the Khondalite Belt in Paleoproterozoic, it is suggested that the Alxa Block should be the western part of the Khondalite Belt in Paleoproterozoic.
- eastern Alxa Block,
- Diebusige Complex,
- late Paleoproterozoic,
- zircon U-Pb dating,
- petrology

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