Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/62505/1/256028a0.pd
AbstractThe East African Rift system (EARS) provides a unique system with the juxtaposition of two c...
International audienceAlthough many continental rifts and passive margins are magmatic, some are not...
[1] The Main Ethiopian Rift (MER) is a classic narrow rift that developed in hot, weak lithosphere, ...
Heat-flow results from eleven widely spaced sites in central and western regions of the Republic of ...
When we look to the world map of heat flow, we see in Africa regions with low heat flow values ( aro...
Most magmatic continental rifts are characterized by surficial expression of magma, which explains t...
I report 26 new heat flow determinations from Tanzania, Zambia, and Zimbabwe which, together with pr...
International audienceThe East African Rift system (EARS) provides a unique system with the juxtapos...
The East African Rift system (EARS) provides a unique system with the juxtaposition of two contrasti...
International audienceAlthough many continental rifts and passive margins are magmatic, some are not...
The Ethiopian Plateau is one of the few tectonically-active regions on Earth that is situated in con...
Although many continental rifts and passive margins are magmatic, some are not1. This observation pr...
We used aeromagnetic and gravity data to investigate the thermal structure beneath the incipient Oka...
International audienceUsing numerical thermo-mechanical experiments we analyze the role of an active...
I report terrestrial heat flow measurements from 25 new sites in Botswana and Namibia. Combining the...
AbstractThe East African Rift system (EARS) provides a unique system with the juxtaposition of two c...
International audienceAlthough many continental rifts and passive margins are magmatic, some are not...
[1] The Main Ethiopian Rift (MER) is a classic narrow rift that developed in hot, weak lithosphere, ...
Heat-flow results from eleven widely spaced sites in central and western regions of the Republic of ...
When we look to the world map of heat flow, we see in Africa regions with low heat flow values ( aro...
Most magmatic continental rifts are characterized by surficial expression of magma, which explains t...
I report 26 new heat flow determinations from Tanzania, Zambia, and Zimbabwe which, together with pr...
International audienceThe East African Rift system (EARS) provides a unique system with the juxtapos...
The East African Rift system (EARS) provides a unique system with the juxtaposition of two contrasti...
International audienceAlthough many continental rifts and passive margins are magmatic, some are not...
The Ethiopian Plateau is one of the few tectonically-active regions on Earth that is situated in con...
Although many continental rifts and passive margins are magmatic, some are not1. This observation pr...
We used aeromagnetic and gravity data to investigate the thermal structure beneath the incipient Oka...
International audienceUsing numerical thermo-mechanical experiments we analyze the role of an active...
I report terrestrial heat flow measurements from 25 new sites in Botswana and Namibia. Combining the...
AbstractThe East African Rift system (EARS) provides a unique system with the juxtaposition of two c...
International audienceAlthough many continental rifts and passive margins are magmatic, some are not...
[1] The Main Ethiopian Rift (MER) is a classic narrow rift that developed in hot, weak lithosphere, ...
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