Focal Mechanisms, Stress Field and Crustal Rheology in the North Tanzanian Divergence (East African Rift) Inferred from Local Seismicity Analysis

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dc.creatorAlbaric, Julie
dc.creatorGodano, Maxime
dc.creatorDéverchère, Jacques
dc.creatorPerrot, Julie
dc.creatorDeschamps, Anne
dc.creatorSue, Christian
dc.creatorLe Gall, Bernard
dc.creatorFerdinand, Richard
dc.creatorPetit, Carole
dc.creatorTiberi, Caterina
dc.date2016-06-13T06:05:57Z
dc.date2016-06-13T06:05:57Z
dc.date2010
dc.date.accessioned2018-03-27T08:57:07Z
dc.date.available2018-03-27T08:57:07Z
dc.descriptionWe deployed a temporary local seismic network in the North Tanzanian Divergence (NTD) for 6 months in 2007 (35 stations, SEISMOTANZ'07 experiment). The region is characterized by major changes in the magmatic/tectonic nature of the rift, at the place where the eastern branch of the East African Rift enters the Tanzanian craton. More than 200 earthquakes were accurately located south of Lake Manyara
dc.identifierAlbaric, J., Godano, M., Déverchere, J., Perrot, J., Deschamps, A., Sue, C., Le Gall, B., Ferdinand, R.W., Petit, C. and Tiberi, C., 2010, May. Focal mechanisms, stress field and crustal rheology in the North Tanzanian Divergence (East African Rift) inferred from local seismicity analysis. In Iceland in the Central Northern Atlantic: hotspot, sea currents and climate change.
dc.identifierhttp://hdl.handle.net/20.500.11810/2431
dc.identifier.urihttp://hdl.handle.net/20.500.11810/2431
dc.languageen
dc.titleFocal Mechanisms, Stress Field and Crustal Rheology in the North Tanzanian Divergence (East African Rift) Inferred from Local Seismicity Analysis
dc.typeJournal Article, Peer Reviewed

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