مشروع البحث:
Structural evolution of continental rifting, quantitative analysis of fault populations: insights from the central Kenya rift, central and north main Ethiopian rift

dc.contributor.advisorThe University of Leeds
dc.date.accessioned2024-12-07T09:07:43Z
dc.date.available2024-12-07T09:07:43Z
dc.descriptionnorthern main Ethiopian rift (NMER), the cumulative distributions for length and displacement populations fit to both exponential and log-normal functions, which is a function of limited crustal layers thickness. The observed decrease of average fault lengths and increasing average fault throws and D/L ratio in the NMER as opposed to the CMER may have occurred after reaching the maximum fault length at an earlier stage of development, which would again be in line with the coherent fault model.
dc.description.abstractAbstract The aim of the current research is to provide new insights into the evolution of normal faults and their implications on continental rift evolution in order to inform our understanding of the north to south rift propagation of the east African rift system (EARS). Therefore, three different rift segments representing different stages of continental rifting have been selected along the EARS
dc.identifier3
dc.identifier.urihttps://dspace.academy.edu.ly/handle/123456789/563
dc.subjectStructural evolution of continental rifting, quantitative analysis of fault populations: insights from the central Kenya rift, central and north main Ethiopian rift
dc.titleStructural evolution of continental rifting, quantitative analysis of fault populations: insights from the central Kenya rift, central and north main Ethiopian rift
dspace.entity.typeProject
project.endDate2018
project.funder.nameالفيزياء
project.investigatorاحمد خليفة مصطفي
project.startDate2017
relation.isOrgUnitOfProject98b1acb9-7c7d-46f0-910e-2228d8f7417b
relation.isOrgUnitOfProject.latestForDiscovery98b1acb9-7c7d-46f0-910e-2228d8f7417b
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