Movement History of the Microcontinents from the Tibetan Plateau Based on Paleomagnetic Results with Sufficient Sampling Units

Yiming Ma; Weimin Ruan; Chao Niu; Tianshui Yang

doi:10.1007/s12583-022-1721-2

Volume 33 Issue 5

Oct 2022

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Journal of Earth Science > 2022 > 33(5): 1072-1080.

Yiming Ma, Weimin Ruan, Chao Niu, Tianshui Yang. Movement History of the Microcontinents from the Tibetan Plateau Based on Paleomagnetic Results with Sufficient Sampling Units. Journal of Earth Science, 2022, 33(5): 1072-1080. doi: 10.1007/s12583-022-1721-2

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Yiming Ma, Weimin Ruan, Chao Niu, Tianshui Yang. Movement History of the Microcontinents from the Tibetan Plateau Based on Paleomagnetic Results with Sufficient Sampling Units. Journal of Earth Science, 2022, 33(5): 1072-1080. doi: 10.1007/s12583-022-1721-2

Citation:

Yiming Ma, Weimin Ruan, Chao Niu, Tianshui Yang. Movement History of the Microcontinents from the Tibetan Plateau Based on Paleomagnetic Results with Sufficient Sampling Units. Journal of Earth Science, 2022, 33(5): 1072-1080. doi: 10.1007/s12583-022-1721-2

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Movement History of the Microcontinents from the Tibetan Plateau Based on Paleomagnetic Results with Sufficient Sampling Units

doi: 10.1007/s12583-022-1721-2

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
College of Earth Sciences, Guilin University of Technology, Guilin 541004, China
3.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China

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Corresponding author: Yiming Ma, maym@cug.edu.cn
Received Date: 20 Apr 2022
Accepted Date: 18 Jul 2022

Available Online: 19 Oct 2022

Issue Publish Date: 30 Oct 2022

Abstract

Abstract

Paleomagnetic results cannot be applied in global and regional tectonic reconstructions unless the paleosecular variation has been adequately averaged. However, how many sampling sites and samples are enough to calculate a reliable paleopole remains debated. Based on the relation among the sampling sites N, the precision parameter k, the virtual geomagnetic pole scatter s, and the confidence limit A₉₅ of the paleopole, we find that 20 sites (samples) or more are required to yield a paleopole with an A₉₅ ≈ 5° based on a review of available paleomagnetic results from the Lhasa, Qiangtang and Tethyan Himalaya. Random samplings of Jurassic virtual geomagnetic poles from the Sangri area show that the Fisher mean pole with neglectable angle deviation can be obtained when sampling sites increase to 20. High-quality paleomagnetic results, with sites/samples number N/n ≥ ~20–30, show that the Qiangtang, Lhasa, and Tethyan Himalaya moved northward in the Late Permian–Middle Triassic, Jurassic, and Cretaceous, respectively, and then accreted to Asia in the Late Triassic, Late Jurassic–Early Cretaceous and Paleocene–Early Eocene, respectively.
- paleolatitude evolution,
- Fisher mean,
- random sampling,
- sampling sites and samples,
- continental collision,
- tectonics

Electronic Supplementary Materials: Supplementary materials (Tables S1–S6) are available in the online version of this article at https://doi.org/10.1007/s12583-022-1721-2.

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References(62)

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Movement History of the Microcontinents from the Tibetan Plateau Based on Paleomagnetic Results with Sufficient Sampling Units

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