大兴安岭南段陆相二叠系-三叠系界线地层序列及其意义:来自锆石U-Pb年代学和生物地层学的证据

张渝金; 张超; 谭红艳; 李伟; 杨晓平; 杨涛; 马永非; 刘淼; 司秋亮; 汪岩

doi:10.3799/dqkx.2019.111

Volume 44 Issue 10

Nov. 2019

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Zhang Yujin, Zhang Chao, Tan Hongyan, Li Wei, Yang Xiaoping, Yang Tao, Ma Yongfei, Liu Miao, Si Qiuliang, Wang Yan, 2019. Advance in Study of Terrestrial Permian-Triassic Boundary Stratigraphic Sequence in Southern Great Xing'an Range and Its Significance: Constraints from Zircon U-Pb Chronology and Biostratigraphy. Earth Science, 44(10): 3314-3332. doi: 10.3799/dqkx.2019.111

Citation:

Zhang Yujin, Zhang Chao, Tan Hongyan, Li Wei, Yang Xiaoping, Yang Tao, Ma Yongfei, Liu Miao, Si Qiuliang, Wang Yan, 2019. Advance in Study of Terrestrial Permian-Triassic Boundary Stratigraphic Sequence in Southern Great Xing'an Range and Its Significance: Constraints from Zircon U-Pb Chronology and Biostratigraphy. Earth Science, 44(10): 3314-3332. doi: 10.3799/dqkx.2019.111

Citation:

Zhang Yujin, Zhang Chao, Tan Hongyan, Li Wei, Yang Xiaoping, Yang Tao, Ma Yongfei, Liu Miao, Si Qiuliang, Wang Yan, 2019. Advance in Study of Terrestrial Permian-Triassic Boundary Stratigraphic Sequence in Southern Great Xing'an Range and Its Significance: Constraints from Zircon U-Pb Chronology and Biostratigraphy. Earth Science, 44(10): 3314-3332. doi: 10.3799/dqkx.2019.111

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Advance in Study of Terrestrial Permian-Triassic Boundary Stratigraphic Sequence in Southern Great Xing'an Range and Its Significance: Constraints from Zircon U-Pb Chronology and Biostratigraphy

doi: 10.3799/dqkx.2019.111

1.
Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
2.
College of Paleontology, Shenyang Normal University, Shenyang 110034, China

Received Date: 2019-05-20
Publish Date: 2019-11-11

Abstract

Abstract

The identification and comparation of terrestrial Permian-Triassic have great significance to the understanding of coeval major global biological and environmental events. In this paper, it focuses on the newly discovered Lower Triassic Laolongtou Formation in Kundu area of Arkhorqin Banner, southern Great Xing'an Range. The contact relationship of Permian-Triassic stratigraphy was studied in particular, plant fossils and palynological fossils above and below the boundary were collected, and the zircon isotopic U-Pb analysis from the volcanic interlayer in the Laolongtou Formation were also analyzed. It is confirmed that there is a parallel unconformity contact relationship between the Laolongtou Formation and the underlying Linxi Formation, and there is a short sedimentary gap between them. The biostratigraphic records show that the Linxi Formation was formed in the Late Permian, however, the Laolongtou Formation was lack of fossil evidence, which may be related to the extinction event at the intersection of the Permian and Triassic. Three isotopes ages from Laolongtou Formation were 251.5±2.2 Ma, 249.7±2.5 Ma and 249.5±1.8 Ma, indicating that they formed at Early Triassic. However, the exact location of the Permian-Triassic boundary needs further study. The Early Triassic magmatic events which widely outcropped at southern Great Xing'an Range area probably related with the closure of Paleo-Asian Ocean. The Paleo-Asian Ocean finally closed along the Xilamulun River suture zone at least until the Early Triassic, and the sedimentary of Laolongtou Formation is the product of collision at its both sides.
- Late Permian,
- Early Triassic,
- Linxi Formation,
- Laolongtou Formation,
- zircon U-Pb chronology,
- biostratigraphy,
- southern Great Xing'an Range

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References(95)

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