Neoproterozoic Diamictite of the Luoquan Formation from the North China Block and Their Implications

Sui, Peishan; Sun, Weidong; Han, Nan; Wang, Lei; Xie, Shucheng; Huang, Zhanpeng; Wang, Xiaohong; Gong, Hongmei; Liu, Jing; Lin, Jian; Xiao, Yuanyuan

doi:10.1007/s12583-021-1550-8

Cited by 2 publications

(1 citation statement)

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“…During the early Middle Permian, the plant fossils in the Yujiabeigou Formation (the zircon age of crystalline tuff was 270 Ma) were all Cathaysian flora molecules, no mixing growth phenomenon, indicating the study area was Cathaysian flora distribution area. At that time, the Solonker-Xar Moron-Changchun-Yanji suture zone was not yet closed (Sun et al,2016), and the PAO developed into an intercontinental residual ocean basin. Subsequently, the oceanic crust disappeared, and continent-continent collision occurred, forming multiple Middle Permian syn-collision granitic intrusions.…”

Section: Middle Permian-continent-continent Collision Environmentmentioning

confidence: 99%

Permian Granitic Plutons from the Northern Margin of the North China Craton: Implications for the Tectonic Evolution of the Central Asian Orogenic Belt

Chen,

Tian,

et al. 2023

Preprint

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As the largest accretionary orogen in the world, the Central Asian Orogenic Belt (CAOB) has continuous juvenile crustal growth in the Phanerozoic. The northern margin of the North China Craton(NCC) and its adjacent area is the eastern segment of the CAOB, and is a key area to study the geological evolution of Paleo-Asian Ocean (PAO). In the Permian, the west of the northern margin of NCC belongs to a post-collision extensional environment, and the east belongs to a subduction stage. But, As a connecting area, the Permian evolution of PAO in the middle of northern margin of NCC has not been systematically studied. In order to fill the blank and understand the temporal and spatial continuous evolution process of PAO, this paper focused on the Permian granitic rocks in the Chifeng area, zircon U-Pb dating and the geochemical analysis of the whole rock main and trace elements were conducted in order to build a granite chronological framework, discuss the genesis and tectonic background of the granite rocks as well as the magma-tectonic evolution history in the Chifeng area. Zircon U-Pb dating results of 8 samples are 269±1 Ma, 268±3 Ma, 260±4 Ma, 260±1 Ma, 260±1 Ma, 255±2 Ma, 254±2 Ma, 256±1Ma, which showed that the Permian granitic rocks had undergone three stages of emplacement: (1) The monzogranite and syenite (294-284 Ma); (2) The monzogranite (269-260Ma) and (3) The monzogranite and syenite (256-254Ma). The Middle Permian magmatism (269-260Ma) was represented by the monzogranite assemblages with different grain sizes. The geochemical characteristics showed that they were high-potassium calc-alkaline-potassium dossonite series of granites formed in compressional environment, indicating there was a collision between the Xing’an-Mongolian Orogenic Belt (XMOB) and the North China Craton (NCC). During the Late Permian-Early Triassic (256-248Ma), the granites in the Chifeng area are dominated by the A-type and I-type granites of high-potassium calc-alkaline series formed under an extensional environments, which constituted typical "bimodal" rock assemblage combined with the coeval basic rocks, suggesting the study area was in an extensional environment where the subducting slab is fragmented during the collision between the XMOB and the NCC. According to emplacement time and occurrence location, the plutons are interpreted to have been generated by the subduction-collision of the Paleo-Asian oceanic crust beneath the NCC. This study provides strong evidence for Permian tectonic evolution and the characterization of the eventual closure of the Paleo-Asian Ocean in the Chifeng City at the northern margin of the NCC.

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Section: Middle Permian-continent-continent Collision Environmentmentioning

confidence: 99%