Cenozoic magmatism throughout east Africa resulting from impact of a single plume¶
Ebinger, & Sleep. (1998). Cenozoic magmatism throughout east Africa resulting from impact of a single plume. Nature.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Uplift
- Magmatic uplift occurs where mantle plumes or large intrusive bodies — batholiths — inject buoyant material into or under the crust, doming the surface; the Colorado Plateau and parts of the East African Rift show this signature.
This sourceShows a single mantle plume beneath the Ethiopian plateau explaining the distribution and timing of magmatism and uplift throughout east Africa.
Supported in partVerified against the work's full text
“Evidence for one or more mantle plumes having impinged beneath the plateaux comes from the dynamic compensation inferred from gravity studies”
- Magmatic uplift occurs where mantle plumes or large intrusive bodies — batholiths — inject buoyant material into or under the crust, doming the surface; the Colorado Plateau and parts of the East African Rift show this signature.
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Registry ID ref:7b787d401517 · see in the full table