中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Paleomagnetism and Ar-Ar geochronology of Cretaceous volcanic rocks in the middle Lhasa terrane, China and tectonic implications

文献类型:期刊论文

作者Tang Xiang-De1,2; Huang Bao-Chun1; Yang Lie-Kun1; Yi Zhi-Yu1; Qiao Qing-Qing1; Chen Li-Wei1,2
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2013
卷号56期号:1页码:136-149
关键词Linzizong Group Lhasa terrane Late Cretaceous Paleomagnetism Ar-Ar dating
ISSN号0001-5733
DOI10.6038/cjg20130114
文献子类Article
英文摘要In order to better understand Cretaceous to Paleogene paleogeography of the Lhasa terrane, 180 drill core samples at 18 sites were collected from Linzizong volcanic rocks near the Coqen town in the middle Lhasa terrane for paleomagnetic studies. Detailed rock magnetic analyses reveal fine-grained ferrimagnetic magnetite as remanence carrier, whilst stepwise thermal and alternating field demagnetizations isolate a high temperature or high field characteristic remanent magnetization (ChRM) from the majority of the sampled rocks. We interpret this characteristic remanence as primary one in the light of a positive fold test result. The ChRM has a tilt-corrected site-mean direction of D=16.2 degrees, I=17.7 degrees with alpha(95)=5.6 degrees, and a corresponding paleopole at 63.1 degrees N, 224.6 degrees E with A(95) = 5.1 degrees. On the other hand, the Ar-Ar dating on three rock samples show that the collected Linzizong volcanic rocks have a geochronological age ranging from similar to 99 to 93 Ma, which is much older than those outcropped in the Linzhou Basin, eastern part of the Lhasa terrane. Then both geochronological and paleomagnetic results reported here indicate a paleolatitude of 8.5 degrees +/- 6.9 degrees N in the Northern Hemisphere for the middle part of the Lhasa terrane during the Late Cretaceous, which is well compatible with those estimated from the Early Paleogene Dianzhong and Nianbo formations in the Linzhou Basin, further indicating that the southernmost margin of the Eurasian continent might have a low paleolatitude of similar to 10 degrees N in the Northern Hemisphere during the Late Cretaceous and Paleocene times. Together with recently published paleomagnetic results for the Paleocene Tethyan Himalayan marine sediments, the low paleolatitudes for Late Cretaceous and,Paleocene Lhasa terrane support the view that the initial contact between India and Asia should be no later than similar to 60.5 Ma. In addition, our results indicate also that at least similar to 1900 km collision-induced crustal shortening should have occurred between the Lhasa terrene and Siberia given that the Eurasian continent behaves as a single rigid plate during the Cenozoic.
WOS关键词INDIA-ASIA COLLISION ; SOUTHERN TIBET ; REMAGNETIZATION CIRCLES ; FOLD TEST ; CONSTRAINTS ; EVOLUTION ; AGE ; BLOCK ; HIMALAYAN ; INITIATION
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000314480100014
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/88082]  
专题中国科学院地质与地球物理研究所
通讯作者Tang Xiang-De
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
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Tang Xiang-De,Huang Bao-Chun,Yang Lie-Kun,et al. Paleomagnetism and Ar-Ar geochronology of Cretaceous volcanic rocks in the middle Lhasa terrane, China and tectonic implications[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2013,56(1):136-149.
APA Tang Xiang-De,Huang Bao-Chun,Yang Lie-Kun,Yi Zhi-Yu,Qiao Qing-Qing,&Chen Li-Wei.(2013).Paleomagnetism and Ar-Ar geochronology of Cretaceous volcanic rocks in the middle Lhasa terrane, China and tectonic implications.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,56(1),136-149.
MLA Tang Xiang-De,et al."Paleomagnetism and Ar-Ar geochronology of Cretaceous volcanic rocks in the middle Lhasa terrane, China and tectonic implications".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 56.1(2013):136-149.

入库方式: OAI收割

来源:地质与地球物理研究所

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