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Long term crustal flow of the Makran subduction zone is computed with a kinematic finite element model based on iterated weighted least squares fits to data. Data include 91 fault traces, 56 fault offset rates, 76 geodetic velocities, 1962 principal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42c625374efe6091a00ccae975932d8a
https://doi.org/10.5194/egusphere-egu2020-864
https://doi.org/10.5194/egusphere-egu2020-864
