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DOI | 10.1016/j.gr.2011.07.019 |
Paleomagnetic results from the Early Cretaceous Zenong Group volcanic rocks, Cuoqin, Tibet, and their paleogeographic implications | |
Chen, Weiwei; Yang, Tianshui; Zhang, Shihong; Yang, Zhenyu; Li, Haiyan; Wu, Huaichun; Zhang, Junhong; Ma, Yiming; Cai, Fulong | |
通讯作者 | Yang, TS (通讯作者) |
发表日期 | 2012 |
ISSN | 1342-937X |
起始页码 | 461 |
结束页码 | 469 |
卷号 | 22期号:2 |
英文摘要 | A paleomagnetic study has been carried out on the Early Cretaceous Zenong Group volcanic rocks (ca. 110 130 Ma) near Cuoqin town in the central Lhasa terrane. Stepwise thermal demagnetization up to 680 degrees C isolated a stable high-temperature component (HTC) including antipodal dual polarities. The HTC directions passed both a fold test at 99% confidence and a reversal test at 95% confidence, suggesting a primary origin. The tilt-corrected average direction for 18 sites is D = 327.0 degrees, I = 35.7 degrees, K = 59.3 degrees, alpha(95) = 4.5 degrees, which corresponds to a paleopole at 58.2 degrees N, 341.9 degrees E (A(95) = 4.6 degrees), yielding a paleolatitude of 19.8 degrees +/- 4.6 degrees N for the study area. Our results, combined with previous paleomagnetic data, suggest that southern Tibet was at a mean paleolatitude of 20 degrees N during the Cretaceous and Paleogene. When compared with the apparent polar wander paths of Asia, the difference suggests that only ca. 870 km north-south crustal shortening has accumulated between the Lhasa terrane and stable Asia since ca. 110 Ma. When comparing the paleolatitudes of the Lhasa terrane and India, the results indicate that the width of the Neotethys was 6720 +/- 690 km during the Early Cretaceous. (c) 2011 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved. |
关键词 | INDIA-ASIA COLLISIONALTYN TAGH FAULTTECTONIC EVOLUTIONLHASA BLOCKGEOMAGNETIC-FIELDSOUTHERN TIBETCENOZOIC TECTONICSMAGNETIC-FIELDLINZHOU BASINWESTERN TIBET |
英文关键词 | Lhasa terrane; Paleomagnetism; Early Cretaceous; Crustal shortening; Neotethys |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000307602000008 |
来源期刊 | GONDWANA RESEARCH |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258038 |
推荐引用方式 GB/T 7714 | Chen, Weiwei,Yang, Tianshui,Zhang, Shihong,et al. Paleomagnetic results from the Early Cretaceous Zenong Group volcanic rocks, Cuoqin, Tibet, and their paleogeographic implications[J]. 中国科学院青藏高原研究所,2012,22(2). |
APA | Chen, Weiwei.,Yang, Tianshui.,Zhang, Shihong.,Yang, Zhenyu.,Li, Haiyan.,...&Cai, Fulong.(2012).Paleomagnetic results from the Early Cretaceous Zenong Group volcanic rocks, Cuoqin, Tibet, and their paleogeographic implications.GONDWANA RESEARCH,22(2). |
MLA | Chen, Weiwei,et al."Paleomagnetic results from the Early Cretaceous Zenong Group volcanic rocks, Cuoqin, Tibet, and their paleogeographic implications".GONDWANA RESEARCH 22.2(2012). |
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