Experimental study on strain field evolution around a simulated thrust faultKey points

Earthquakes result from continuous geodynamic processes. A topic of significant interest for the scientific community is to elaborate on the phenomena governing the faulting and fracturing of crustal rocks. Therefore, in this study, uniaxial compressive shear failure experiments were conducted on Fa...

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Main Authors: Yonghong Zhao, Yanjun Xiao, Jiaying Yang, Xiaofan Li, Andong Xu
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2023-02-01
Series:Earthquake Science
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S167445192300006X
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author Yonghong Zhao
Yanjun Xiao
Jiaying Yang
Xiaofan Li
Andong Xu
author_facet Yonghong Zhao
Yanjun Xiao
Jiaying Yang
Xiaofan Li
Andong Xu
author_sort Yonghong Zhao
collection DOAJ
description Earthquakes result from continuous geodynamic processes. A topic of significant interest for the scientific community is to elaborate on the phenomena governing the faulting and fracturing of crustal rocks. Therefore, in this study, uniaxial compressive shear failure experiments were conducted on Fangshan marble rock samples with a prefabricated slot to simulate thrust faulting. The center of each marble plate (105 mm × 80 mm × 5 mm) was engraved with a 30-mm long double-sided nonpenetrating slot (depth: 2 mm, width: 0.5 mm). The deformation and destruction processes of the rock surface were recorded using a high-speed camera. The digital image correlation method was used to calculate the displacement and strain distribution and variation at different loading stages. The accumulative and incremental displacement fields u and v, strain field ex and ey, and shear strain exy were analyzed. When the loading level reached its ultimate value, the strain field was concentrated around the prefabricated slot. The concentration reached a maximum at the ends of the prefabricated slot. The magnitude of shear strain reached 0.1. This experiment contributes to our understanding of the dynamic process of active faulting.
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spelling doaj.art-3fc4ff5836e449eaa22c3f11c9c3f7212023-03-24T04:22:09ZengKeAi Communications Co., Ltd.Earthquake Science1867-87772023-02-013614051Experimental study on strain field evolution around a simulated thrust faultKey pointsYonghong Zhao0Yanjun Xiao1Jiaying Yang2Xiaofan Li3Andong Xu4School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaState Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 100083, China; SinoPEC Key Laboratory of Seismic Elastic Wave Technology, Beijing 100083, China; SinoPEC Petroleum Exploration and Production Research Institute, Beijing 100083, ChinaSchool of Earth and Space Sciences, Peking University, Beijing 100871, China; Corresponding author: yang_jiaying@pku.edu.cnSchool of Earth and Space Sciences, Peking University, Beijing 100871, ChinaSchool of Earth and Space Sciences, Peking University, Beijing 100871, ChinaEarthquakes result from continuous geodynamic processes. A topic of significant interest for the scientific community is to elaborate on the phenomena governing the faulting and fracturing of crustal rocks. Therefore, in this study, uniaxial compressive shear failure experiments were conducted on Fangshan marble rock samples with a prefabricated slot to simulate thrust faulting. The center of each marble plate (105 mm × 80 mm × 5 mm) was engraved with a 30-mm long double-sided nonpenetrating slot (depth: 2 mm, width: 0.5 mm). The deformation and destruction processes of the rock surface were recorded using a high-speed camera. The digital image correlation method was used to calculate the displacement and strain distribution and variation at different loading stages. The accumulative and incremental displacement fields u and v, strain field ex and ey, and shear strain exy were analyzed. When the loading level reached its ultimate value, the strain field was concentrated around the prefabricated slot. The concentration reached a maximum at the ends of the prefabricated slot. The magnitude of shear strain reached 0.1. This experiment contributes to our understanding of the dynamic process of active faulting.http://www.sciencedirect.com/science/article/pii/S167445192300006Xexperimental studydeformation field evolutionfracture processearthquake
spellingShingle Yonghong Zhao
Yanjun Xiao
Jiaying Yang
Xiaofan Li
Andong Xu
Experimental study on strain field evolution around a simulated thrust faultKey points
Earthquake Science
experimental study
deformation field evolution
fracture process
earthquake
title Experimental study on strain field evolution around a simulated thrust faultKey points
title_full Experimental study on strain field evolution around a simulated thrust faultKey points
title_fullStr Experimental study on strain field evolution around a simulated thrust faultKey points
title_full_unstemmed Experimental study on strain field evolution around a simulated thrust faultKey points
title_short Experimental study on strain field evolution around a simulated thrust faultKey points
title_sort experimental study on strain field evolution around a simulated thrust faultkey points
topic experimental study
deformation field evolution
fracture process
earthquake
url http://www.sciencedirect.com/science/article/pii/S167445192300006X
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AT yanjunxiao experimentalstudyonstrainfieldevolutionaroundasimulatedthrustfaultkeypoints
AT jiayingyang experimentalstudyonstrainfieldevolutionaroundasimulatedthrustfaultkeypoints
AT xiaofanli experimentalstudyonstrainfieldevolutionaroundasimulatedthrustfaultkeypoints
AT andongxu experimentalstudyonstrainfieldevolutionaroundasimulatedthrustfaultkeypoints