DOI: 10.1007/s00531-014-1032-7
论文题名: Detrital zircon U-Pb ages of Late Triassic-Late Jurassic deposits in the western and northern Sichuan Basin margin: Constraints on the foreland basin provenance and tectonic implications
作者: Luo L. ; Qi J.-F. ; Zhang M.-Z. ; Wang K. ; Han Y.-Z.
刊名: International Journal of Earth Sciences
出版年: 2014
卷: 103, 期: 6 起始页码: 1553
结束页码: 1568
语种: 英语
英文关键词: LA-ICP-MS
; Qinling
; Sichuan Basin
; U-Pb detrital zircon
; Xujiahe
Scopus关键词: depocenter
; detrital deposit
; foreland basin
; geochronology
; Jurassic
; paleogeography
; provenance
; sandstone
; Triassic
; uranium-lead dating
; zircon
; China
; Sichuan Basin
英文摘要: Upper Triassic to Upper Jurassic strata in the western and northern Sichuan Basin were deposited in a synorogenic foreland basin. Ion-microprobe U-Pb analysis of 364 detrital zircon grains from five Late Triassic to Late Jurassic sandstone samples in the northern Sichuan Basin and several published Middle Triassic to Middle Jurassic samples in the eastern Songpan-Ganzi Complex and western and inner Sichuan Basin provide an initial framework for understanding the Late Triassic to Late Jurassic provenance of western and northern Sichuan Basin. For further understanding, the paleogeographic setting of these areas and neighboring hinterlands was constructed. Combined with analysis of depocenter migration, thermochronology and detrital zircon provenance, the western and northern Sichuan Basin is displayed as a transferred foreland basin from Late Triassic to Late Jurassic. The Upper Triassic Xujiahe depocenter was located at the front of the Longmen Shan belt, and sediments in the western Sichuan Basin shared the same provenances with the Middle-Upper Triassic in the Songpan-Ganzi Complex, whereas the South Qinling fed the northern Sichuan Basin. The synorogenic depocenter transferred to the front of Micang Shan during the early Middle Jurassic and at the front of the Daba Shan during the middle-late Middle Jurassic. Zircons of the Middle Jurassic were sourced from the North Qinling, South Qinling and northern Yangtze Craton. The depocenter returned to the front of the Micang Shan again during the Late Jurassic, and the South Qinling and northern Yangtze Craton was the main provenance. The detrital zircon U-Pb ages imply that the South and North China collision was probably not finished at the Late Jurassic. © 2014 Springer-Verlag Berlin Heidelberg. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84906327019&doi=10.1007%2fs00531-014-1032-7&partnerID=40&md5=530f548cdd7db9d42d8be2a1db0d7f35
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70450
Appears in Collections: 影响、适应和脆弱性 气候减缓与适应
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作者单位: State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing, 102249, China; College of Geosciences, China University of Petroleum, Beijing, 102249, China; School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210093, China
Recommended Citation:
Luo L.,Qi J.-F.,Zhang M.-Z.,et al. Detrital zircon U-Pb ages of Late Triassic-Late Jurassic deposits in the western and northern Sichuan Basin margin: Constraints on the foreland basin provenance and tectonic implications[J]. International Journal of Earth Sciences,2014-01-01,103(6)