DOI: 10.1016/j.tecto.2021.228965
论文题名: Early Triassic initial collision between the North China and South China blocks in the eastern Qinling Orogenic Belt
作者: Ma Q. ; Yang J. ; Du Y. ; Dai X. ; Chai R. ; Guo H. ; Xu Y.
刊名: Tectonophysics
ISSN: 00401951
出版年: 2021
卷: 814 语种: 英语
中文关键词: Continental collision
; Mesozoic
; Qinling Orogenic Belt
; Sedimentary provenance
; South China
英文关键词: Silicate minerals
; Stratigraphy
; Subsidence
; Zircon
; Continental collisions
; Jialingjiang formation
; North China blocks
; Qinling orogenic belts
; Recycled materials
; Slope environments
; South China block
; Tectonic uplift
; Tectonics
; collision zone
; continental collision
; orogenic belt
; Permian-Triassic boundary
; petrography
; plate motion
; plate tectonics
; provenance
; tectonic setting
; Triassic
; China
; North China Block
; Qinling Belt
; South China Block
英文摘要: The closure of Mianlue Ocean lead to the collisional assembly between the North China Block (NCB) and the South China Block (SCB). But the timing of initial continental collision remains unclear, with the proposed ages ranging from the Late Permian to the Late Triassic. This study presents stratigraphic, sedimentological, tectonic subsidence, and provenance data from the Triassic strata in the Zigui and Dangyang basins lying along the eastern Qinling Orogenic Belt. These data document a tectonic transition in the central northern-SCB, and locally provide constraints on the timing of initial SCB–NCB collision. The Lower Triassic Daye Formation was deposited in a marginal basin to slope environment, and consists of mudrocks containing detrital zircons with major age peaks at ca. 1900 and 850 Ma. The overlying Lower Triassic Jialingjiang Formation comprises a shallowing carbonate sequence, with intercalated evaporites at the top of the formation. It contains mudrocks that are rich in detrital zircons with of ca. 270‐–245 Ma. The mixed carbonate and siliciclastic sequences of the Middle–Upper Triassic Badong Formation records tectonic uplift at its base, and contains detrital zircons with U[sbnd]Pb age peaks at ca. 2500, 1850, 920–800, 450 and 350–220 Ma. Combined with petrographical observations and tectonic subsidence calculation, these detrital zircon U[sbnd]Pb ages record a significant provenance change from recycled material derived from the SCB to newly generated detrital material from the NCB. This provenance change records the initial SCB–NCB collision in the eastern Qinling Orogenic Belt during the Early Triassic. © 2021 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/170856
Appears in Collections: 气候变化与战略
There are no files associated with this item.
作者单位: State Key Laboratory of Biogeology and Environmental Geology & School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China
Recommended Citation:
Ma Q.,Yang J.,Du Y.,et al. Early Triassic initial collision between the North China and South China blocks in the eastern Qinling Orogenic Belt[J]. Tectonophysics,2021-01-01,814