T009
From deep lithosphere to earth surface process; the natural laboratory of the east African rift
From deep lithosphere to earth surface process; the natural laboratory of the east African rift
Session ID#: 161414
Session Description:
The East African rift represents a natural laboratory where deep sourced thermo-chemical anomaly could be linked to early phase of plateau uplift, magmatism and rifting in East Africa. Those mechanisms are enhancing depositional processes shaping the continental slope of the western Indian Ocean but also changing the topography of East Africa, reorganizing river catchments, drainage basins, and moderating climate. However to date, the relationship between EARS seismicity, magmatism and the instability of the continental margin of East Africa is still poorly known, on both long-term and short-term time scales. The tectonic processes triggering the offshore evolution of the Somali plate (or western Indian Ocean) are still very elusive due to both the complex microplate kinematics and their poorly defined tectonic boundary nowadays by active extensional structures. We welcome submissions from modern seismology, geodesy, paleogeodesy, geophysics, geochemistry and geology along with advances in modelling capabilities aiming at revealing the details of these processes affecting the East African region.
Index Terms:
3002 Continental shelf and slope processes [MARINE GEOLOGY AND GEOPHYSICS]
8038 Regional crustal structure [STRUCTURAL GEOLOGY]
8120 Dynamics of lithosphere and mantle: general [TECTONOPHYSICS]
8178 Tectonics and magmatism [TECTONOPHYSICS]
Primary Convener: David Iacopini, The University of Naples Federico II, DISTAR, Naples, Italy
Conveners: Vittorio Maselli, Dalhousie University, Department of Earth and Environmental Sciences, Halifax, NS, Canada, Cynthia J Ebinger, Tulane University, School of Science & Engineering, New Orleans, LA, United States and Jolante van Wijk, New Mexico Institute of Mining and Technology, Earth & Environmental Science, Socorro, NM, United States
See more of: Tectonophysics
