المؤلفون: Muluneh A.A.[1, Brune S.[2, Illsley-Kemp F.[4], Corti G.[5], Keir D.[6, Glerum A.[2], Kidane T.[1, Mori J.[9]

المصدر: Geochemistry, geophysics, geosystems 21 (2020): 1–13. doi:10.1029/2020GC008935
info:cnr-pdr/source/autori:Muluneh A.A.[1,2], Brune S.[2,3],Illsley-Kemp F.[4], Corti G.[5], Keir D.[6,7], Glerum A.[2], Kidane T.[1,8], Mori J.[9]/titolo:Mechanism for Deep Crustal Seismicity: Insight From Modeling of Deformation Processes at the Main Ethiopian Rift/doi:10.1029%2F2020GC008935/rivista:Geochemistry, geophysics, geosystems/anno:2020/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:21
Geochemistry Geophysics Geosystems (G3)

مصطلحات موضوعية: Rift, 010504 meteorology & atmospheric sciences, Numerical modeling, Deformation (meteorology), Strain rate, Induced seismicity, 010502 geochemistry & geophysics, 01 natural sciences, earthquakes, deep crust, Ethiopian rift, Geophysics, Geochemistry and Petrology, Mechanism (sociology), Geology, Seismology, Main Ethiopian Rift (MER), 0105 earth and related environmental sciences

وصف الملف: application/pdf; text

URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::673be6a17015928a19b99abc5f4307ef
https://publications.cnr.it/doc/462890