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Normal left-oblique fault mechanisms as an indication of sinistral deformation between the Nubia and Somalia Plates in the Main Ethiopian Rift
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2000 (English)In: JOURNAL OF AFRICAN EARTH SCIENCES, ISSN 0899-5362, Vol. 31, no 2, 359-367 p.Article in journal (Refereed) Published
Abstract [en]

Four regional earthquakes were studied for source parameters and focal mechanisms in the Main Ethiopian Rift. The results show normal faulting with significant left-lateral strike-slip components for all of the studied earthquakes. The horizontal componen

Place, publisher, year, edition, pages
PERGAMON-ELSEVIER SCIENCE LTD , 2000. Vol. 31, no 2, 359-367 p.
Keyword [en]
MOMENT TENSOR RETRIEVAL; WAVE-FORM INVERSION; EAST-AFRICAN; SOURCE PARAMETERS; AFAR DEPRESSION; RED-SEA; EARTHQUAKES; SYSTEM; SEISMICITY; KINEMATICS
Identifiers
URN: urn:nbn:se:uu:diva-37800OAI: oai:DiVA.org:uu-37800DiVA: diva2:65699
Note
Addresses: Ayele A, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden. Dept Earth Sci, S-75236 Uppsala, Sweden. Univ Addis Ababa, Fac Sci, Geophys Observ, Addis Ababa, Ethiopia.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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