Abstract: Transient deformation in the Asal-Ghoubbet Rift (Djibouti) since the 1978 diking event: Is deformation controlled by magma supply rates? (2016 AGU Fall Meeting)

Transient deformation in the Asal-Ghoubbet Rift (Djibouti) since the 1978 diking event: Is deformation controlled by magma supply rates?

Delphine Smittarello, ISTerre Institute of Earth Sciences, Saint Martin d'Hères, France, Raphael Grandin, Université de Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France, Jean-Bernard de Chabalier, Institut de Physique du Globe de Paris, Paris, France, Cecile Doubre, Université de Strasbourg, IPGS, École et Observatoire des Sciences de la Terre, Strasbourg, France, Aline Deprez, École et Observatoire des Sciences de la Terre, Institut Terre et Environnement de Strasbourg, Centre National de la Recherche Scientifique, University of Strasbourg, Strasbourg, France, Frederic Masson, Univ Strasbourg, Strasbourg Cedex, France, Anne Socquet, University Grenoble Alpes, ISTerre Institute of Earth Sciences, Grenoble, France and Saad Ibrahim Ahmed, Geophysical Observatory of Arta, Arta, Djibouti

Back to: One Rift, Two Rift, Magma-Rich Rift, Magma-Poor Rift: Deformation, Magmatism, Volatile Fluxes, and Their Consequences in the East African Rift System II