Effective Normal Stress is the difference between the total normal stress acting across a fault plane and the pore fluid pressure within the rock matrix, representing the portion of the applied stress that is effectively borne by the solid framework of the fault and thus governs frictional resistance to shear failure.
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Planetary Science Institute
Tucson, United States
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Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
13 h-index
25 publications
2.3K citations
United States Geological Survey
Reston, United States
12 h-index
22 publications
1.7K citations
Utrecht University
Utrecht, The Netherlands
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Pennsylvania State University
State College, United States
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The University of Texas at Austin
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- Journal of Geophysical Research Atmospheres
JGR · 31 publications · 6K citations
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- Journal of Geophysical Research Solid Earth
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- Geophysical Research Letters
32 publications · 2K citations
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- Géotechnique
13 publications · 984 citations
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- Journal of Geotechnical and Geoenvironmental Engineering
12 publications · 818 citations
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