| Citation: |
XU Xinyue, YUAN Zhaode, SHAO Yanxiu, LIU Jing, YAO Wenqian, LI Wenqiao, HAN Longfei. Paleo-earthquake evidence and its quantitative evaluationin trenches:Exemplified by active strike-slip faults[J]. Geological Bulletin of China, 2019, 38(6): 977-992.
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Paleo-earthquake evidence and its quantitative evaluationin trenches:Exemplified by active strike-slip faults
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Abstract
Identification of paleo-earthquake events in trench depends on the interpretation of the structural deformations and associated sedimentary responses preserved in the sedimentary strata. Based on 88papers of paleoseismic studies of strike-slip fault published in China and abroad, the authors systematically summarized the empirical paleoseismic indicators, which includes vertical offset, upward termination of fault, growth strata, infilled fissures, angular unconformities, liquefactions, colluvial wedges and folds. The quality and frequency of these event indicators constitute the key to distinguishing paleoseismic events and event horizons. Ground deformation caused by non-structuralfactor and creepingis slightly different from eventindicators.In practice, the semiquantitative methodcan minimize the influence of non-seismic genetic deformations, reduce the risk of misestimating of paleoearthquake events, and give an objective event confidence level.
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Keywords:
- strike-slip fault /
- paleoearthquake trench /
- paleoearthquake /
- event indicators /
- creeping
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References
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XU Xinyue, YUAN Zhaode, SHAO Yanxiu, LIU Jing, YAO Wenqian, LI Wenqiao, HAN Longfei. Paleo-earthquake evidence and its quantitative evaluationin trenches:Exemplified by active strike-slip faults[J]. Geological Bulletin of China, 2019, 38(6): 977-992.
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Figure 1.
Various patterns of surface rupture produced by strike-slip earthquakes
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Figure 2.
Statistical features of the paleo-earthquake event indicators
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Figure 3.
Typical paleoearthquake evidence on strike-slip faults
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Figure 4.
The event indicator rank of paleo-earthquake events of the copper mine trench on the Altun fault
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Figure 5.
Quantitative histograms of paleo-earthquake event indicators of the copper mine trench on the Altun fault