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- W2088392705 startingPage "885" @default.
- W2088392705 abstract "Suswa volcano, located at 1°10′S, 36°20′E, is Quaternary in age ( Following caldera I collapse, phonolite lava flows were erupted from the caldera floor. Centrally-erupted phonolite lava flows led to the construction of Ol Doinyo Onyoke lava cone. A pit-crater on the cone was a precursor to the collapse of caldera II, both of which were generated entirely by magma withdrawal. Regional decompression caused ring-fault bounded, block-resurgence of the caldera floor" @default.
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- W2088392705 date "1993-09-01" @default.
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- W2088392705 title "Incremental caldera collapse of Suswa volcano, Gregory Rift Valley, Kenya" @default.
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- W2088392705 doi "https://doi.org/10.1144/gsjgs.150.5.0885" @default.
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