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This page is a summary of: Transient Aseismic Slip Following 2017 Mw 7.3 Sarpol-e Zahab, Iran, Earthquake: Possible Evidence for Fault Frictional Heterogeneity and Thin-skinned Shortening Following a Thick-skinned Basement-involved Faulting in the Zagros Fold-thrust Belt, November 2021, Wiley,
DOI: 10.1002/essoar.10508853.1.
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