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The subduction-accretion history of the Bangong-Nujiang Ocean: Constraints from provenance and geochronology of the Mesozoic strata near Gaize, central Tibet
Li, S (Li, Shun)1,2; Ding, L (Ding, Lin)2,3; Guilmette, C (Guilmette, Carl)1; Fu, JJ (Fu, Jiajun)4; Xu, Q (Xu, Qiang)2,3; Yue, YH (Yue, Yahui)2; Henrique-Pinto, R (Henrique-Pinto, Renato)1; Li, S
Source PublicationTECTONOPHYSICS
2017
Volume702Issue:0Pages:42-60
DOI10.1016/j.tecto.2017.02.023
AbstractThe Mesozoic strata, within the Bangong-Nujiang suture zone in central Tibet, recorded critical information about the subduction-accretion processes of the Bangong-Nujiang Ocean prior to the Lhasa-Qiangtang collision. This paper reports detailed field observations, petrographic descriptions, sandstone detrital zircon U-Pb ages and Hf isotopic analyses from an accretionary complex (preserved as Mugagangri Group) and the unconformably overlying Shamuluo Formation near Gaize. The youngest detrital zircon ages, together with other age constraints from literature, suggest that the Mugagangri Group was deposited during late Triassic-early Jurassic, while the Shamuluo Formation was deposited during late Jurassic-early Cretaceous. Based on the differences in lithology, age and provenance, the Mugagangri Group is subdivided into the upper, middle and lower subunits. These units are younging structurally downward/southward, consistent with models of progressive off-scrapping and accretion in a southward-facing subduction complex. The upper subunit, comprising mainly quartz-sandstone and siliceous mud/shale, was deposited in abyssal plain environment close to the Qiangtang passive margin during late Triassic, with sediments derived from the southern Qiangtang block. The middle and lower subunits comprise mainly lithic-quartz-sandstone and mud/shale, containing abundant ultramafic/ophiolitic fragments. The middle subunit, of late Triassic-early Jurassic age, records a transition in tectono-depositional setting from abyssal plain to trench-wedge basin, with sudden influx of sediments sourced from the central Qjangtang metamorphic belt and northern Qjangtang magmatic belt. The appearance of ultramafic/ophiolitic fragments in the middle subunit reflects the subduction initiation. The lower subunit was deposited in a trench-wedge basin during early Jurassic, with influx of Jurassic-aged zircons originating from the newly active southern Qiangtang magmatic arc. The lower subunit records the onset of arc magmatism related to the northward subduction of the Bangong-Nujiang Ocean. The Shamuluo Formation, comprising mainly lithic-feldspar-sandstone with limestone interlayers, was deposited in a post-collisional residual-sea or pre-collisional trench-slope basin, with sediments derived entirely from the Qiangtang block. (C) 2017 Elsevier B.V. All rights reserved.
Subject Area地质学
WOS IDWOS:000399511100005
Language英语
Indexed BySCI
KeywordZIRCON U-PB PALEO-TETHYS OCEAN TRIASSIC ARC MAGMATISM SOUTHERN TIBET TECTONIC EVOLUTION NEO-TETHYS LHASA TERRANE OROGENIC BELT WESTERN CHINA LU-HF
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics ; Geochemistry & Geophysics
Cooperation Status国际
Citation statistics
Cited Times:25[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/8262
Collection图书馆
Corresponding AuthorLi, S
Affiliation1.Univ Laval, Dept Geol & Genie Geol, 1065 Ave Med, Quebec City, PQ G1V 0A6, Canada.
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China.
3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China.
4.Fujian Inst Geol Survey, Fuzhou 350013, Peoples R China.
Recommended Citation
GB/T 7714
Li, S ,Ding, L ,Guilmette, C ,et al. The subduction-accretion history of the Bangong-Nujiang Ocean: Constraints from provenance and geochronology of the Mesozoic strata near Gaize, central Tibet[J]. TECTONOPHYSICS,2017,702(0):42-60.
APA Li, S .,Ding, L .,Guilmette, C .,Fu, JJ .,Xu, Q .,...&Li, S.(2017).The subduction-accretion history of the Bangong-Nujiang Ocean: Constraints from provenance and geochronology of the Mesozoic strata near Gaize, central Tibet.TECTONOPHYSICS,702(0),42-60.
MLA Li, S ,et al."The subduction-accretion history of the Bangong-Nujiang Ocean: Constraints from provenance and geochronology of the Mesozoic strata near Gaize, central Tibet".TECTONOPHYSICS 702.0(2017):42-60.
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