Distribution of Quaternary deformation in the central Main Ethiopian Rift, East Africa
Author:
Affiliation:
1. Consiglio Nazionale delle Ricerche; Istituto di Geoscienze e Georisorse, U.O. Firenze; Florence; Italy
2. Dipartimento di Scienze della Terra; Università degli Studi di Firenze; Florence; Italy
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/tc/tc1104/2010TC002833/2010TC002833.pdf
Reference51 articles.
1. Abebe , T. P. Manetti M. Bonini G. Corti F. Innocenti F. Mazzarini Z. Pècksay 2005 Geological map (scale 1:200.000) of the northern Main Ethiopian Rift and its implications for the volcano-tectonic evolution of the rift Map and Chart MCH094 Geol. Soc. of Am. Boulder, Colo. 10.1130/2005MCH094TXT
2. The central Main Ethiopian Rift is younger than 8 Ma: Confirmation through Apatite fission-track thermochronology;Abebe;Terra Nova,2010
3. Holocene extension direction along the Main Ethiopian Rift, East Africa;Acocella;Terra Nova,2002
4. Formation of normal faults along the axial zone of the Ethiopian rift;Acocella;J. Struct. Geol.,2003
5. Evolution, pattern, and partitioning of deformation during oblique continental rifting: Inferences from lithospheric-scale centrifuge models;Agostini;Geochem. Geophys. Geosyst.,2009
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