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Deformational History of the Kanguer Subduction Complex in the Eastern Tianshan (NW China): Implications for Paleozoic-Triassic Multiple Accretionary Tectonics of the Southern Altaids
Mao, Qigui1,2,3; Xiao, Wenjiao1,3,4,5; Buckman, Solomon6; Huang, Peng1,3,4; Ao, Songjian3,4; Song, Dongfang3,4; Zhang, Ji'en3,4; Sang, Miao1,3; Tan, Zhou1,3; Wang, Hao1,3; Li, Rui1,3
2022-11-01
Source PublicationTECTONICS
ISSN0278-7407
Volume41Issue:11Pages:31
AbstractThe Kanguer Subduction Complex in the Eastern Tianshan is critical to understanding the tectonic evolution of the southern Altaids as it marks the terminal suture along which the Paleo-Asian Ocean was consumed. However, the nature and timing of this final collision, as well as the mechanism of shearing and related magmatism, remain enigmatic. The Kanguer Subduction Complex demonstrates obvious sinistral transtensional and dextral compressional deformation in different tectonic events along the Qiugemingtash Shear Zone in Huangshan area. Three sets of asymmetric plunging folds (e.g., basin-like, S-shaped and Z(W)-shaped) were recognized in the sedimentary rocks. Locally, the folds are offset by dextral strike-slip faults, indicating that they were formed by dextral shearing. The Huangshandong mafic-ultramafic complex experienced brittle dextral shearing partitioned around the margins of the intrusion. Detrital zircon U-Pb dates for deformed sedimentary rocks have maximum deposit ages (MDA) of 251 and 290 Ma, respectively, and syn-compressional shearing conjugate granitic dikes that intruded into the deformed sedimentary rocks yield crystallization ages of 249 and 245 Ma, respectively. These ages reveal that the extensional and/or transtensional sedimentary basins formed between ca. 290-249 Ma, and dextral compressional shearing started ca. 249 Ma. Combining deformed units with transtensional basins and mantle-derived magmatism, we suggest that ocean-ridge subduction induced a sinistral transtensional regime in a forearc/intraarc setting related to the Tuva-Mongol Orocline in the Permian. The oblique convergence between the Tarim Craton and southern Altaids triggered the Qiugemingtash dextral compressional shearing in the Early Triassic (ca. 249 Ma).
KeywordKanguer Subduction Complex Qiugemingtash Shear Zone folds Permian transtension orocline Eastern Tianshan
DOI10.1029/2022TC007527
WOS KeywordMAFIC-ULTRAMAFIC INTRUSIONS ; U-PB CHRONOLOGY ; MO DEPOSIT ; CENTRAL-ASIA ; NORTHWEST CHINA ; OROGENIC BELT ; GOLD DEPOSIT ; HF ISOTOPES ; GEOCHEMISTRY ; EVOLUTION
Language英语
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics
WOS IDWOS:000888585600001
PublisherAMER GEOPHYSICAL UNION
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Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/107656
Collection岩石圈演化国家重点实验室
Corresponding AuthorMao, Qigui; Xiao, Wenjiao; Tan, Zhou
Affiliation1.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, Xinjiang Inst Ecol & Geog, Urumqi, Peoples R China
2.Redrock Min CO Ltd, Hami, Peoples R China
3.Natl Key Lab Ecol Secur & Resource Utilizat Arid, Urumqi, Peoples R China
4.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing, Peoples R China
5.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
6.Univ Wollongong, Sch Earth & Environm Sci, Wollongong, NSW, Australia
Recommended Citation
GB/T 7714
Mao, Qigui,Xiao, Wenjiao,Buckman, Solomon,et al. Deformational History of the Kanguer Subduction Complex in the Eastern Tianshan (NW China): Implications for Paleozoic-Triassic Multiple Accretionary Tectonics of the Southern Altaids[J]. TECTONICS,2022,41(11):31.
APA Mao, Qigui.,Xiao, Wenjiao.,Buckman, Solomon.,Huang, Peng.,Ao, Songjian.,...&Li, Rui.(2022).Deformational History of the Kanguer Subduction Complex in the Eastern Tianshan (NW China): Implications for Paleozoic-Triassic Multiple Accretionary Tectonics of the Southern Altaids.TECTONICS,41(11),31.
MLA Mao, Qigui,et al."Deformational History of the Kanguer Subduction Complex in the Eastern Tianshan (NW China): Implications for Paleozoic-Triassic Multiple Accretionary Tectonics of the Southern Altaids".TECTONICS 41.11(2022):31.
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