Building a Multilake Paleoseismometer for the Xianshuihe Fault (Tibetan Plateau, China)
- 4 December 2024
- journal article
- research article
- Published by American Geophysical Union (AGU) in Tectonics
- Vol. 43 (12)
Abstract
The Xianshuihe fault, located in the southeastern Tibetan Plateau, stands as one of the most active faults in China. As assessing earthquake hazard relies on access to long‐term paleoseismological archives, this paper seeks to optimize the interpretation of paleoseismological records. We retrieved nine sediment cores from three lakes over a 30 km fault segment. Earthquake‐related deposits were identified through grain‐size analysis, XRF core scanning, and SEM observations of thin sections. Age models based on short‐lived radionuclides correlate these events with historical earthquakes, which are recorded with varying sensitivities to seismic intensity across the three lakes. We developed a code that evaluates the plausibility of rupture scenarios against sedimentary evidence: Each site is used as a binary paleoseismometer, indicating whether or not an earthquake reached a local intensity threshold. The combined evidence from the three sites allows to evaluate rupture scenarios on the Xianshuihe fault, according to rupture length‐magnitude scaling laws and intensity prediction equations. The most probable scenarios allow to discriminate the rupture area and magnitude range providing a good agreement with historical reconstructions. Our work demonstrates the potential of combining earthquake records to infer the magnitude and rupture zone of paleo‐earthquakes, even with a limited data set. Our approach, applicable across diverse geological settings and timescales, offers enhanced precision in understanding long‐term paleoseismology covering multiple earthquake cycles. However, establishing the synchronicity of events in such an active area—where earthquake return times are typically <100 years—demands highly accurate age models, which remains challenging.Keywords
All Related Versions
Funding Information
- China Geological Survey, Ministry of Natural Resources (DD20240041)
- National Key Research and Development Program of China (2023YFC3012003)
- Agence Nationale de la Recherche (ANR‐20‐CE49‐0008)
This publication has 54 references indexed in Scilit:
- Time-dependent recurrence of strong earthquake shaking near plate boundaries: A lake sediment perspectiveEarth-Science Reviews, 2020
- Investigation and magnitude re‐evaluation of the 1955 Zheduotang earthquake, eastern Tibetan Plateau, ChinaGeological Journal, 2019
- Southeastward increase of the late Quaternary slip-rate of the Xianshuihe fault, eastern Tibet. Geodynamic and seismic hazard implicationsEarth and Planetary Science Letters, 2018
- Quantified sensitivity of small lake sediments to record historic earthquakes: Implications for paleoseismologyJournal of Geophysical Research: Earth Surface, 2015
- Prediction of Geochemical Composition from XRF Core Scanner Data: A New Multivariate Approach Including Automatic Selection of Calibration Samples and Quantification of Uncertainties2015
- Lake sediments record high intensity shaking that provides insight into the location and rupture length of large earthquakes on the Alpine Fault, New ZealandEarth and Planetary Science Letters, 2014
- Lacustrine turbidites as a tool for quantitative earthquake reconstruction: New evidence for a variable rupture mode in south central ChileJournal of Geophysical Research: Solid Earth, 2014
- Structural interpretation of the great earthquakes of the last millennium in the central HimalayaEarth-Science Reviews, 2013
- Rupture history of the 2013 Mw 6.6 Lushan earthquake constrained with local strong motion and teleseismic body and surface wavesGeophysical Research Letters, 2013
- Estimation of coseismic deformation and a fault model of the 2010 Yushu earthquake using PALSAR interferometry dataEarth and Planetary Science Letters, 2011