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Co-Seismic Surface Rupture and Recurrence Interval of Large Earthquakes along Damaoyaba-litang Segment of the litang fault on the Eastern Margin of the Tibetan Plateau in China

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Journal of Earth Science 2021年第5期32卷 1139-1151页

作者： Shiyuan Wang Rongjun Zhou Mingjian Liang Shao Liu Nina Liu Jianyu Long Sichuan Earthquake Agency^Chengdu 610041 China School of Geological Engineering and Geomatics Chang'an UniversityXi'an 710054China

The litang fault is a left-lateral secondary shear zone in the Sichuan-Yunnan active block that accommodates the tectonic deformation associated with the eastward extrusion of the upper crust of the Tibetan Plateau. Based on 1 : 50 000 geological mapping of active faults, the litang fault consists of three geometric segments, the Cuopuhu, Damaoyaba, and litang segments, in the west of litang, which are divided by the of Haizi Mountain uplift and the wide-angle bending and branching of the fault near Jinchanggou. This study also identifies the surface rupture of the A.D. 1890 earthquake, which is distributed intermittently along the ~28 km long Damaoyaba segments and ~25 km long litang segments. The maximum horizontal displacement is 4.1 m along Damaoyaba segments, and 4 m along litang segments. The rupture involves typical left-lateral shear movement. The two ruptures are divided by discontinuous segments or gaps that are ~18 km long;thus, the total surface rupture is approximately 71 km long. The estimated moment magnitude was M_(w)7.3±0.1. A comprehensive analysis of data obtained from 5 trenches excavated along the Damaoyaba and litang segments and the trench data by Xu et al.(2005) identifies age constraints of the 4 most recent paleoseimic events occurred B.C. 1468±54–1340±25, B.C. 52±25–A.D. 76±47, A.D. 1115±90, and A.D. 1890, respectively. The recurrence intervals are 1 415±80, 1 104±104, and 775±90 a, which are consistent with quasi-periodic earthquake recurrence behavior. The average recurrence interval is 1 098±112 a.

关键词： litang fault surface rupture active fault recurrence intervals paleoearthquake eastern Tibetan Plateau

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A palaeoearthquake event and its age revealed by the travertine layer along the litang fault in the southeastern margin of the Qinghai-Tibetan plateau

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Earthquake Research Advances 2023年第3期3卷 53-62页

作者： Yao Yang Mingjian Liang Chao Ma Jun Li Hualiang Shen Fang Du Song Luo Shao Liu Xuelian Rui Sichuan Earthquake Agency Chengdu610041China College of Earth Sciences Chengdu University of TechnologyChengdu610059China Zhejiang Earthquake Agency Hangzhou310013China Chengdu Geological Survey Center China Geological SurveyChengdu610081China

The litang fault(LTF),located in the southeast of the Qinghai-Tibetan Plateau,is known for its high level of present-day seismicity,whereas its Pleistocene activity has been scarcely documented.This study focused on a tract of banded travertine deposits precipitated from thermal waters along the NW–SE-trending LTF trace.The role of travertine deposits in recording neotectonic activity has been studied by identifying their internal structure.Typical soft-sediment deformation structures observed within the banded travertines include micro folds,liquefied breccia,and liquefied diapirs.These deformed structures,which are restricted to a single unit separated unconformably by undeformed layers,can be traced for tens of meters,indicating that they were formed by seismic shaking triggered by LTF activity.The deformation of the banded travertine layers is attributed to the combined effects of seismic shaking,liquefaction,and fluidization,and it can be related to a paleo earthquake event with a magnitude of MS>5.The U-series ages obtained from the banded travertine deposits perturbed by the earthquakes are in the range of 130.59–112.94 ka,indicating an important fault-assisted neotectonic activity that occurred during the Middle–Late Pleistocene.Analysis of such structures,in combination with the use of U-series dating methods,can yield a reliable timing of neotectonic activity and provide new evidence for under-standing the seismotectonic setting of the litang area.

关键词： Travertine Paleoearthquake Soft-sediment deformation U-series dating litang fault

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