2018
DOI: 10.1007/s00024-018-1800-6
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Background Stress State Before the 2008 Wenchuan Earthquake and the Dynamics of the Longmen Shan Thrust Belt

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Cited by 6 publications
(1 citation statement)
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“…Studies on the sub-instable stage utilized the migration of small earthquakes on the fault plane, cross-fault baseline and level, rate of crustal movement, water levels of confined aquifers near the fault zone, etc. (e.g., Wang et al, 2018;Zhang et al, 2020;Huang et al, 2021;Wang et al, 2021;Ma et al, 2022). The continuous accumulation of stress on a fault at the late seismogenic stage ought to be accompanied by stratum deformation and changes in physical property parameters.…”
Section: Introductionmentioning
confidence: 99%
“…Studies on the sub-instable stage utilized the migration of small earthquakes on the fault plane, cross-fault baseline and level, rate of crustal movement, water levels of confined aquifers near the fault zone, etc. (e.g., Wang et al, 2018;Zhang et al, 2020;Huang et al, 2021;Wang et al, 2021;Ma et al, 2022). The continuous accumulation of stress on a fault at the late seismogenic stage ought to be accompanied by stratum deformation and changes in physical property parameters.…”
Section: Introductionmentioning
confidence: 99%