Lithospheric thickness beneath the southern Kenya Rift: implications from basalt geochemistry
Geochemical data are reported for samples from the flanks and floor of the soutehrn Kenya Rift Valley in the Lake Magadi darea, and from two central volcanoes located within the rift valley. Rift lavas include samples of Singaraini and O1 Tepesi basalts on the eastern flank, Kirikiti basalts from th...
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| Veröffentlicht in: | Contributions to mineralogy and petrology 2001-10, Vol.142 (1), p.89-106 |
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| container_title | Contributions to mineralogy and petrology |
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| creator | Roex, Anton P. Späth, Andreas Zartman, Robert E. |
| description | Geochemical data are reported for samples from the flanks and floor of the soutehrn Kenya Rift Valley in the Lake Magadi darea, and from two central volcanoes located within the rift valley. Rift lavas include samples of Singaraini and O1 Tepesi basalts on the eastern flank, Kirikiti basalts from the western flank, and plateau trachytes from the rift valley floor. |
| doi_str_mv | 10.1007/s004100100273 |
| format | Article |
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| ispartof | Contributions to mineralogy and petrology, 2001-10, Vol.142 (1), p.89-106 |
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| language | eng |
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| subjects | Basalt Geochemistry Geology Lava Mineralogy Petrology Rift valleys Trace elements Volcanoes |
| title | Lithospheric thickness beneath the southern Kenya Rift: implications from basalt geochemistry |
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