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DOI | 10.1016/j.tecto.2021.228965 |
Early Triassic initial collision between the North China and South China blocks in the eastern Qinling Orogenic Belt | |
Ma Q.; Yang J.; Du Y.; Dai X.; Chai R.; Guo H.; Xu Y. | |
发表日期 | 2021 |
ISSN | 00401951 |
卷号 | 814 |
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. |
关键词 | Continental collisionMesozoicQinling Orogenic BeltSedimentary provenanceSouth 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 |
语种 | 英语 |
来源期刊 | Tectonophysics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/208023 |
作者单位 | State Key Laboratory of Biogeology and Environmental Geology & School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China |
推荐引用方式 GB/T 7714 | 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],2021,814. |
APA | Ma Q..,Yang J..,Du Y..,Dai X..,Chai R..,...&Xu Y..(2021).Early Triassic initial collision between the North China and South China blocks in the eastern Qinling Orogenic Belt.Tectonophysics,814. |
MLA | Ma Q.,et al."Early Triassic initial collision between the North China and South China blocks in the eastern Qinling Orogenic Belt".Tectonophysics 814(2021). |
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