Zobrazeno 1 - 10
of 20
pro vyhledávání: '"R. Kounoudis"'
Autor:
M. Musila, C. J. Ebinger, I. D. Bastow, G. Sullivan, S. J. Oliva, E. Knappe, M. Perry, R. Kounoudis, C. S. Ogden, R. Bendick, S. Mwangi, N. Mariita, G. Kianji, E. Kraus, F. Illsley‐Kemp
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 9, Pp n/a-n/a (2023)
Abstract The role of lithospheric heterogeneities, presence or absence of melt, local and regional stresses, and gravitational potential energy in strain localization in continental rifts remains debated. We use new seismic and geodetic data to ident
Externí odkaz:
https://doaj.org/article/ca5a8266de9b4dc488b45e41d16c93b9
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 8, Pp n/a-n/a (2023)
Abstract Ethiopia's Cenozoic flood basalt magmatism, uplift, and rifting have been attributed to one or more mantle plumes. The Nubian plate, however, has drifted 500–1,000 km north since initial magmatism at ∼45 Ma, having developed above mantle
Externí odkaz:
https://doaj.org/article/a24df4652ea5451098bfeac563afb505
Autor:
R. Kounoudis, I. D. Bastow, C. J. Ebinger, C. S. Ogden, A. Ayele, R. Bendick, N. Mariita, G. Kianji, G. Wigham, M. Musila, B. Kibret
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021)
Abstract The Turkana Depression, a topographically subdued, broadly rifted zone between the elevated East African and Ethiopian plateaus, disrupts the N–S, fault‐bounded rift basin morphology that characterizes most of the East African Rift. The
Externí odkaz:
https://doaj.org/article/3c932a2f184d40cc98c71952897fe7ff
Autor:
A. Boyce, I. D. Bastow, S. Cottaar, R. Kounoudis, J. Guilloud De Courbeville, E. Caunt, S. Desai
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 3, Pp n/a-n/a (2021)
Abstract Africa's Cenozoic tectonism is often attributed to mantle plumes, particularly below East Africa, but their morphology, number, location, and impact on the African lithosphere are debated. The broad slow wavespeed African Superplume, ubiquit
Externí odkaz:
https://doaj.org/article/231e28a5d5974bcebe7fbf66b64158d1
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 7, Pp n/a-n/a (2020)
Abstract The Eastern Mediterranean captures the east‐west transition from active subduction of Earth's oldest oceanic lithosphere to continental collision, making it an ideal location to study terminal‐stage subduction. Asthenospheric‐ or subdu
Externí odkaz:
https://doaj.org/article/3814749b387e487ca01004af5d7d7c9d
Autor:
C.S. Ogden, I.D. Bastow, C. Ebinger, A. Ayele, R. Kounoudis, M. Musila, R. Bendick, N. Mariita, G. Kianji, T.O. Rooney, G. Sullivan, B. Kibret
Publikováno v:
Earth and Planetary Science Letters. 609:118088
The Turkana Depression in Eastern Africa separates the elevated plateaus of East Africa to the south and Ethiopia-Yemen to the north. It remains unclear whether the Depression lacks dynamic mantle support, or if the entire East Africa region is dynam
The subdued topography of the Turkana Depression separates the elevated Ethiopian and Kenyan Plateaus in East Africa. Mechanisms to explain its topography are debated because constraints on upper m...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f83e94900a7fed035656a01ad7febf2
https://doi.org/10.1002/essoar.10508941.1
https://doi.org/10.1002/essoar.10508941.1
The eastern Mediterranean hosts, within the span of a few hundred kilometers, extensional, strike-slip, and collision tectonics above a set of fragmenting subducting slabs. Slab roll-back, toroidal flow, and lithospheric dripping/delamination process
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b34be6ca7c0873366f58b7ab2ca87cdc
http://hdl.handle.net/10044/1/90935
http://hdl.handle.net/10044/1/90935
Autor:
Cynthia Ebinger, Ian D. Bastow, M. Musila, R. Kounoudis, Atalay Ayele, B. A. Kibret, C. S. Ogden, Rebecca Bendick, Nicholas Mariita, G. Wigham, G. Kianji
The Turkana Depression, a topographically-subdued, broadly-rifted zone between the elevated East African and Ethiopian plateaus, disrupts the N–S, fault-bounded rift basin morphology that characterizes most of the East African Rift. The unusual bre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::73661577720d27ae70b8c7d558e1ffbe
http://hdl.handle.net/10044/1/90652
http://hdl.handle.net/10044/1/90652
Autor:
E. Caunt, Sanne Cottaar, S. Desai, R. Kounoudis, J. Guilloud De Courbeville, Ian D. Bastow, A. Boyce
Africa’s Cenozoic tectonism is often attributed to mantle plumes, particularly below East Africa, but their morphology, number, location, and impact on the African lithosphere are debated. The broad slow wavespeed African Superplume, ubiquitous in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5a7de40343c7e6475504139c5d41389c