Earthquakes

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$Downdip component of strain rate tensor and resolved stress difference from the numerical model, focusing on features within the plate/slab. The resolved stress difference is defined as ($\sigma_{s} - \sigma_{z}$), where $\hat{s}$, and $\hat{z}$ are unit vectors in the downdip and slab normal directions. The fields show, for example, shortening/extension in the downdip direction. Stress profiles at four locations are shown. The blue line ($x_0$) is the first zero crossing based on analysis of the flexural component of the topography. The black line is the location of maximum bending moment.$

Plate bending earthquakes and the strength distribution of the lithosphere

Uploaded by: Dan Sandiford

Uploaded: May 28, 2024

Software: ASPECT v2.4.0

Tags:

C++Dynamics of lithosphere Earthquakes Lithospheric flexure Subduction adaptive-mesh-refinement finite-element particles

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