Tectonic development of the western branch of the East African rift system¶
Ebinger. (1989). Tectonic development of the western branch of the East African rift system.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Rift Zone
- In the south (Malawi/Tanzania segments), extension is young and distributed: broad thermal doming and scattered normal faulting, amagmatic in large part
This sourceA structural study of the western branch of the East African rift system showing high-angle border-fault basins with crustal extension under 15% and volcanism beginning about 7 Ma in the south.
Supported in partVerified against the publisher's abstract
“The Western rift, the western branch of the East African rift system, is bordered by high-angle normal fault systems bounding one side of spoon-shaped basins.”
- In the south (Malawi/Tanzania segments), extension is young and distributed: broad thermal doming and scattered normal faulting, amagmatic in large part
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Registry ID ref:06427163d67d · see in the full table