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.contributor.authorAlbaric, Julie
dc.contributor.authorGodano, Maxime
dc.contributor.authorDéverchère, Jacques
dc.contributor.authorPerrot, Julie
dc.contributor.authorDeschamps, Anne
dc.contributor.authorSue, Christian
dc.contributor.authorLe Gall, Bernard
dc.contributor.authorFerdinand, Richard W.
dc.contributor.authorPetit, Carole
dc.contributor.authorTiberi, Caterina
dc.date.accessioned2016-06-13T06:05:57Z
dc.date.available2016-06-13T06:05:57Z
dc.date.issued2010
dc.description.abstractWe 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 Manyaraen_US
dc.identifier.citationAlbaric, 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.en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11810/2431
dc.language.isoenen_US
dc.titleFocal Mechanisms, Stress Field and Crustal Rheology in the North Tanzanian Divergence (East African Rift) Inferred from Local Seismicity Analysisen_US
dc.typeJournal Article, Peer Revieweden_US
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