中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
An Inclination Shallowing-Corrected Early Triassic Paleomagnetic Pole for the North China Craton: Implication for the Mesozoic Geography of Proto-Asia

文献类型:期刊论文

作者Zhao, Pan1,2,3; Appel, Erwin2; Xu, Bei4
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2020-10-01
卷号125期号:10页码:21
ISSN号2169-9313
DOI10.1029/2020JB019489
英文摘要The Early Mesozoic is a key period for the formation of the Asia continent. In this study, in order to reconstruct the Early Mesozoic paleogeography of Proto-Asia, we carried out a paleomagnetic study on the Early Triassic strata from the Chengde Basin in the northeastern North China Craton (NCC). Rock magnetic investigations reveal magnetite and hematite as the main magnetic carriers. Characteristic remanent magnetization directions from 21 sites show normal and reversed polarities and site-mean directions pass fold tests. After inclination shallowing (IS) correction with the elongation/inclination method, a mean direction is calculated at D-s/I-s = 322.5 degrees/39.5 degrees (k(s) = 32.6, alpha(95s) = 5.7 degrees) in stratigraphic coordinates. The corresponding Early Triassic paleomagnetic pole (lambda/phi = 53.5 degrees N/9.5 degrees E, A(95) = 5.3 degrees) overlaps with coeval poles that have also been corrected for IS reported from the western part of the NCC. This result indicates that there is no relative movement between the eastern and western parts of the NCC. With all IS-corrected paleomagnetic poles, a mean Early Triassic pole is recalculated for the NCC at lambda/ phi= 59.4 degrees N/13.4 degrees E (A(95) = 4.7 degrees). We use this pole to reconstruct the paleogeography of Proto-Asia and confirm previous studies that did not use IS corrections, in which two "triangle bay-shaped" oceans, the Paleo-Tethys Ocean and the Mongol-Okhotsk Ocean, existed along the southern and northern margins of the unified NCC-Mongolian Block (MOB). Clockwise rotations of the South China Craton and Siberia Craton relative to the NCC-MOB during the Early Mesozoic led to the final closure of both oceans.
WOS关键词EASTERN INNER-MONGOLIA ; TECTONIC EVOLUTION ; XIABANCHENG BASIN ; SHANXI PROVINCE ; SIBERIAN TRAPS ; OROGENIC BELT ; OKHOTSK OCEAN ; WANDER PATH ; SOUTH CHINA ; TIME-SCALE
资助项目National Key R&D Program of China[2017YFC0601302] ; National Nature Science Foundation of China[41888101] ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Alexander von Humboldt Foundation ; University Tubingen, Germany
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000604458900060
出版者AMER GEOPHYSICAL UNION
资助机构National Key R&D Program of China ; National Key R&D Program of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Alexander von Humboldt Foundation ; Alexander von Humboldt Foundation ; University Tubingen, Germany ; University Tubingen, Germany ; National Key R&D Program of China ; National Key R&D Program of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Alexander von Humboldt Foundation ; Alexander von Humboldt Foundation ; University Tubingen, Germany ; University Tubingen, Germany ; National Key R&D Program of China ; National Key R&D Program of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Alexander von Humboldt Foundation ; Alexander von Humboldt Foundation ; University Tubingen, Germany ; University Tubingen, Germany ; National Key R&D Program of China ; National Key R&D Program of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Chinese Academy of Sciences Pioneer Hundred Talents Program ; Alexander von Humboldt Foundation ; Alexander von Humboldt Foundation ; University Tubingen, Germany ; University Tubingen, Germany
源URL[http://ir.iggcas.ac.cn/handle/132A11/99983]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Zhao, Pan
作者单位1.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China
2.Univ Tubingen, Dept Geosci, Tubingen, Germany
3.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing, Peoples R China
4.Hebei GEO Univ, Coll Earth Sci, Shijiazhuang, Hebei, Peoples R China
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Zhao, Pan,Appel, Erwin,Xu, Bei. An Inclination Shallowing-Corrected Early Triassic Paleomagnetic Pole for the North China Craton: Implication for the Mesozoic Geography of Proto-Asia[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2020,125(10):21.
APA Zhao, Pan,Appel, Erwin,&Xu, Bei.(2020).An Inclination Shallowing-Corrected Early Triassic Paleomagnetic Pole for the North China Craton: Implication for the Mesozoic Geography of Proto-Asia.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,125(10),21.
MLA Zhao, Pan,et al."An Inclination Shallowing-Corrected Early Triassic Paleomagnetic Pole for the North China Craton: Implication for the Mesozoic Geography of Proto-Asia".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 125.10(2020):21.

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来源:地质与地球物理研究所

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