Structural patterns and ages of Permian-Triassic multistage strike-slip faulting in the Chifeng area, southeastern Inner Mongolia, China: Implications for the final closure of the Paleo-Asian Ocean

Yang, Qian; Shi, Wei; Li, Xiaogang; Wang, Tianyu; Lin, Mao

doi:10.1016/j.jseaes.2024.106006

Cited by 1 publication

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“…During this period, the left-lateral strike-slip motion in the northern TLFZ cut across the CKF (the original boundary between the NCC and CAOB), leading to a segmentation of the Dunhua-Mishan Fault (DMF) between the two offsetting CKF portions, forming the boundary between the NCC and CAOB (Gu et al, 2018;Xu et al, 2000). Despite extensive research on the geometric, kinematic, and dynamic characteristics of the CKF, the exact location of the spatial contact of this boundary between the NCC and CAOB remains heavily debated (Liu et al, 2019;Q. Yang et al, 2024) because of limited rock exposure and extensive Cenozoic sediment coverage.…”

Section: Introductionmentioning

confidence: 99%

Fine Crust‐Mantle Structure of the Major Tectonic Boundaries Between the North China Craton and Central Asian Orogenic Belt Revealed From Rayleigh Wave Phase Velocities and Receiver Functions

Yang,

Xu,

et al. 2024

JGR Solid Earth

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The Tanlu Fault Zone (TLFZ) and Chifeng‐Kaiyuan Fault (CKF) serve as tectonic boundaries between the North China Craton (NCC) and the Central Asian Orogenic Belt (CAOB). Clarifying the refined structure of these tectonic boundaries is crucial for understanding the relationships between the tectonic units and the heterogeneity in the destruction of the NCC. In this study, two linear seismic arrays were deployed across these tectonic boundaries. Based on the phase velocity dispersion and receiver functions extracted from the seismic arrays, the Hamiltonian Monte Carlo algorithm was employed for the joint inversion of the S‐wave velocity (Vs) in the crust and uppermost mantle. The Vs model was then used to correct the time differences in common conversion point (CCP) stacking. The CCP stacking results indicate that the boundary faults TLFZ and CKF are both whole‐crustal faults that separate the NCC and CAOB. The Vs structure showed a significant low‐velocity anomaly in the mantle beneath the NCC, with intense seismic activity within the crust. This suggests that the NCC was affected by the subduction of the Western Pacific, leading to crustal and mantle destruction. In contrast, the CAOB exhibited a clear high‐velocity anomaly with relatively stable crustal structures. We believe that the NCC and CAOB have undergone structural modification and destruction due to the closure of the Paleo‐Asian Ocean and the activities of the TLFZ since the Late Mesozoic. During the Cenozoic, the region east of the TLFZ experienced more significant destruction in the NCC than the other adjacent tectonic units.

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