IGGCAS OpenIR  > 矿产资源研究院重点实验室
Timing of the Kaiyuan-Jiapigou shear zone in the northern margin of the North China Craton: Implications for closure of the Mongol-Okhotsk Ocean
Huang, Shi-Qi1; Dong, Shu-Wen1,2; Zhang, Fochin3; Zhang, Yue-Qiao2; Shi, Wei4; Mueller, Werner E. G.5
2022-12-05
Source PublicationTECTONOPHYSICS
ISSN0040-1951
Volume844Pages:19
AbstractThe ductile Kaiyuan-Jiapigou Shear Zone (KJSZ) is located within the eastern part of the northern margin of the North China Craton (NCC). The foliation within the shear zone generally dips at 55 degrees towards N20 degrees and contains a lineation that plunges at 40 degrees towards N30 degrees. Field and thin section observations and quartz c-axis fabrics of the KJSZ indicate that this zone records top-to-the-SSW shearing associated with a NNE-SSW regional compression event. Muscovite, biotite, and hornblende 40Ar/39Ar step-heating ages constrain the timing of shearing and the tectonothermal history of the KJSZ. Quartz c-axis fabrics and mineral deformation features indicate the defor-mation within the KJSZ occurred at temperatures of 400 degrees C-450 degrees C, which are lower than the Ar-Ar closure temperature of hornblende but higher than the closure temperatures of muscovite and biotite. Samples from the KJSZ yield 40Ar/39Ar step-heating ages from 164.6 +/- 0.5 to 165.2 +/- 0.6 Ma for hornblende samples and from 161.4 +/- 0.4 to 163.1 +/- 0.4 Ma for mica samples. Combining these ages with the temperature of deformation within the KJSZ indicates that this shear zone most likely formed between 165.2 +/- 0.6 and 161.4 +/- 0.4 Ma. Linking these new data with the tectonics and geochronology of the eastern part of the northern margin of the NCC suggests that the deformation within this region was most likely controlled by a nearly N-S compressional event associated with the far field effect of the Mongol-Okhotsk Ocean closure during the Middle-Late Jurassic.
KeywordKaiyuan-Jiapigou Shear Zone Deformation 40Ar 39Ar age Middle-Late Jurassic Mongol-Okhotsk Ocean
DOI10.1016/j.tecto.2022.229626
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; Deep Exploration of China ; Deep Exploration of China ; National Key RD Plan ; National Key RD Plan ; China Geological Survey Project ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; Operating Expenses of Basic Scientific Research Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Deep Exploration of China ; Deep Exploration of China ; National Key RD Plan ; National Key RD Plan ; China Geological Survey Project ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; Operating Expenses of Basic Scientific Research Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Deep Exploration of China ; Deep Exploration of China ; National Key RD Plan ; National Key RD Plan ; China Geological Survey Project ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; Operating Expenses of Basic Scientific Research Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Deep Exploration of China ; Deep Exploration of China ; National Key RD Plan ; National Key RD Plan ; China Geological Survey Project ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; Operating Expenses of Basic Scientific Research Project
WOS KeywordLU FAULT ZONE ; PRESSURE CONTINENTAL-CRUST ; METAMORPHIC CORE COMPLEX ; 40AR/39AR MINERAL AGES ; ASIAN OROGENIC BELT ; GREAT XINGAN RANGE ; EAST CENTRAL CHINA ; NE CHINA ; TECTONIC EVOLUTION ; U-PB
Language英语
Funding ProjectNational Natural Science Foundation of China ; Deep Exploration of China ; National Key RD Plan ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; [41702218] ; [SinoProbe-08-01] ; [2017YFC0601402] ; [DD20190010] ; [JKY202126]
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; Deep Exploration of China ; Deep Exploration of China ; National Key RD Plan ; National Key RD Plan ; China Geological Survey Project ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; Operating Expenses of Basic Scientific Research Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Deep Exploration of China ; Deep Exploration of China ; National Key RD Plan ; National Key RD Plan ; China Geological Survey Project ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; Operating Expenses of Basic Scientific Research Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Deep Exploration of China ; Deep Exploration of China ; National Key RD Plan ; National Key RD Plan ; China Geological Survey Project ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; Operating Expenses of Basic Scientific Research Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Deep Exploration of China ; Deep Exploration of China ; National Key RD Plan ; National Key RD Plan ; China Geological Survey Project ; China Geological Survey Project ; Operating Expenses of Basic Scientific Research Project ; Operating Expenses of Basic Scientific Research Project
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics
WOS IDWOS:000890424400003
PublisherELSEVIER
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/107641
Collection矿产资源研究院重点实验室
Corresponding AuthorDong, Shu-Wen
Affiliation1.Chinese Acad Geol Sci, Beijing, Peoples R China
2.Nanjing Univ, Sch Earth Sci & Engn, Nanjing, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
4.Chinese Acad Geol Sci, Inst Geomech, Beijing, Peoples R China
5.Johannes Gutenberg Univ Mainz, Univ Med Ctr, Mainz, Germany
Recommended Citation
GB/T 7714
Huang, Shi-Qi,Dong, Shu-Wen,Zhang, Fochin,et al. Timing of the Kaiyuan-Jiapigou shear zone in the northern margin of the North China Craton: Implications for closure of the Mongol-Okhotsk Ocean[J]. TECTONOPHYSICS,2022,844:19.
APA Huang, Shi-Qi,Dong, Shu-Wen,Zhang, Fochin,Zhang, Yue-Qiao,Shi, Wei,&Mueller, Werner E. G..(2022).Timing of the Kaiyuan-Jiapigou shear zone in the northern margin of the North China Craton: Implications for closure of the Mongol-Okhotsk Ocean.TECTONOPHYSICS,844,19.
MLA Huang, Shi-Qi,et al."Timing of the Kaiyuan-Jiapigou shear zone in the northern margin of the North China Craton: Implications for closure of the Mongol-Okhotsk Ocean".TECTONOPHYSICS 844(2022):19.
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