NDLI: Paleomagnetic results from Late Carboniferous to Early Permian rocks in the northern Qiangtang terrane, Tibet, China, and their tectonic implications

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Pyrite morphology and episodic euxinia of the Ediacaran Doushantuo Formation in South China

Evaluation of Pt and Au pressure scales based on MgO absolute pressure scale

Paleomagnetic results from Late Carboniferous to Early Permian rocks in the northern Qiangtang terrane, Tibet, China, and their tectonic implications

Late Glacial glacier-climate modeling in two valleys on the eastern slope of Samdainkangsang Peak, Nyaiqentanggulha Mountains

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Paleomagnetic results from Late Carboniferous to Early Permian rocks in the northern Qiangtang terrane, Tibet, China, and their tectonic implications

Content Provider	Springer Nature Link
Author	Yang, XingFeng Cheng, Xin Zhou, YaNan Ma, Lun Zhang, XiaoDong Yan, ZhaoSheng Peng, XiMing Su, HaiLun Wu, HanNing
Copyright Year	2016
Abstract	Results of a systematic paleomagnetic study are reported based on Late Carboniferous to Early Permian sedimentary rocks on the north slope of the Tanggula Mountains, in the northern Qiangtang terrane (NQT), Tibet, China. Data revealed that magnetic minerals in limestone samples from the Zarigen Formation (CP^z)are primarily composed of magnetite, while those in sandstone samples from the Nuoribagaribao Formation (Pnr) are dominated by hematite alone, or hematite and magnetite in combination. Progressive thermal, or alternating field, demagnetization allowed us to isolate a stable high temperature component (HTC) in 127 specimens from 16 sites which successfully passed the conglomerate test, consistent with primary remnance. The tilt-corrected mean direction for Late Carboniferous to Early Permian rocks in the northern Qiangtang terrane is D $_{s}$=30.2°, I $_{s}$=- 40.9°, k $_{s}$=269.0, α $_{95}$=2.3°, N=16, which yields a corresponding paleomagnetic pole at 25.7°N, 241.5°E (dp/dm=2.8°/1.7°), and a paleolatitude of 23.4°S. Our results, together with previously reported paleomagnetic data, indicate that: (1) the NQT in Tibet, China, was located at a low latitude in the southern hemisphere, and may have belonged to the northern margin of Gondwana during the Late Carboniferous to Early Permian; (2) the Paleo-Tethys Ocean was large during the Late Carboniferous to Early Permian, and (3) the NQT subsequently moved rapidly northwards, perhaps related to the fact that the Paleo-Tethys Ocean was rapidly contracting from the Late Permian to Late Triassic while the Bangong Lake-Nujiang Ocean, the northern branch of the Neo-Tethys Ocean, expanded rapidly during this time.
Starting Page	124
Ending Page	134
Page Count	11
File Format	PDF
ISSN	16747313
Journal	Science in China Series D: Earth Sciences
Volume Number	60
Issue Number	1
e-ISSN	18691897
Language	English
Publisher	Science China Press
Publisher Date	2016-09-20
Publisher Place	Beijing
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Northern Qiangtang terrane Late Carboniferous Early Permian Rock magnetism Conglomerate test Paleomagnetic pole Earth Sciences
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences

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