Silicic central volcanoes as precursors to rift propagation: the Afar case

Details Silicic central volcanoes as precursors to rift propagation: the Afar case Silicic central volcanoes as precursors to rift propagation: the Afar case

Feb 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003e%26psl.207..103l&link_type=abstract

Earth and Planetary Science Letters, Volume 207, Issue 1-4, p. 103-116.

Mathematics

Logic

14

Afar, Rift Propagation, Silicic Volcanism, Geochronology, Aden Ridge, Red Sea Ridge

Scientific paper

The Afar depression is a triple junction characterised by thinned continental crust, where three rift systems meet (Red Sea, Gulf of Aden and East African Rift). About 100 recent K-Ar ages obtained on Plio-Pleistocene lavas [Lahitte et al., J. Geophys. Res. (2002) in press; Kidane et al., J. Geophys. Res. (2002) in press], complemented by new geomorphological interpretations, allow better understanding of the volcano-tectonic activity linked to rift propagation. In Central Afar, a significant spatial and temporal correlation is observed between the occurrence of silicic central volcanoes and the initiation of the successive phases of on-land propagation of the Red Sea and Aden rifts. Inside the Afar depression, at the scale of both a whole ridge and a small rift segment, silicic lavas are systematically erupted close to the location of a future rift segment and prior to the main extensive phase associated with fissural basaltic activity. Central silicic volcanoes therefore appear to be precursor features, and their locations underline the preferred direction of future rift propagation. Evolved volcanoes (and associated magma chambers) form zones of localised lithospheric weakness, which concentrate stress and guide the development of fractures in which fissural magmatism is next emplaced. Differentiated silicic lavas are erupted first. Then, as extension increases, basaltic magma directly erupts to the surface. This composite style of rifting, with volcanic and tectonic components, is a scaled-down equivalent of the continental break-up process at the largest scale.

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