Relevant bibliographies by topics / North Tanzanian Divergence

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  2. Dissertations / Theses

Academic literature on the topic 'North Tanzanian Divergence'

Author: Grafiati
Published: 4 June 2021
Last updated: 17 February 2022

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Journal articles on the topic "North Tanzanian Divergence"

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Mana, Sara, Tanya Furman, Brent D. Turrin, Mark D. Feigenson, and Carl C. Swisher. "Magmatic activity across the East African North Tanzanian Divergence Zone." Journal of the Geological Society 172, no. 3 (2015): 368–89. http://dx.doi.org/10.1144/jgs2014-072.

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Plasman, Matthieu, Sophie Hautot, Pascal Tarits, et al. "Lithospheric Structure of a Transitional Magmatic to Amagmatic Continental Rift System—Insights from Magnetotelluric and Local Tomography Studies in the North Tanzanian Divergence, East African Rift." Geosciences 9, no. 11 (2019): 462. http://dx.doi.org/10.3390/geosciences9110462.

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Continental break-up is controlled by several parameters and processes (rheology, inherited structures, magmatism, etc). Their impact, chronology and interactions are still poorly known and debated, particularly when rifting interacts with cratons. In order to better understand the rifting initiation in a cratonic lithosphere, we analysed 22 magnetotelluric (MT) soundings collected along two East-West profiles in two different rift segments of the North Tanzanian Divergence. The North Tanzanian Divergence, where the East African Rift is at its earliest stage, is a remarkable example of the tra
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Parisi, Laura, Ian Stanistreet, Jackson Njau, Kathy Schick, Nicholas Toth, and Paul Martin Mai. "Seismological Investigations in the Olduvai Basin and Ngorongoro Volcanic Highlands (Western Flank of the North Tanzanian Divergence)." Seismological Research Letters 91, no. 6 (2020): 3286–303. http://dx.doi.org/10.1785/0220200111.

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Abstract We present data and results of a passive seismic experiment that we operated between June 2016 and May 2018 in the Ngorongoro Conservation Area (northern Tanzania), located on the western side of the eastern branch of the Eastern African Rift (EAR) system. The motivation for this experiment is twofold: (1) investigating the extension of the Olduvai basin, referred to also as the “Cradle of Human Mankind,” as it hosted a variety of paleoenvironments exploited by hominins during their evolution; and (2) studying the link between the fault system in the main EAR and in its western flank.
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4

Dobrynina, A. A., J. Albaric, A. Deschamps, et al. "Seismic wave attenuation in the lithosphere of the North Tanzanian divergence zone (East African rift system)." Russian Geology and Geophysics 58, no. 2 (2017): 253–65. http://dx.doi.org/10.1016/j.rgg.2016.03.016.

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Le Gall, Bernard, Remigius Gama, Alexander Koptev, et al. "The anomalously-propagating South Kenya rift in the context of the North Tanzanian Divergence zone, East Africa." Tectonophysics 814 (September 2021): 228968. http://dx.doi.org/10.1016/j.tecto.2021.228968.

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Albaric, J., J. Perrot, J. Déverchère, et al. "Contrasted seismogenic and rheological behaviours from shallow and deep earthquake sequences in the North Tanzanian Divergence, East Africa." Journal of African Earth Sciences 58, no. 5 (2010): 799–811. http://dx.doi.org/10.1016/j.jafrearsci.2009.09.005.

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7

Mana, S., T. Furman, M. J. Carr, et al. "Geochronology and geochemistry of the Essimingor volcano: Melting of metasomatized lithospheric mantle beneath the North Tanzanian Divergence zone (East African Rift)." Lithos 155 (December 2012): 310–25. http://dx.doi.org/10.1016/j.lithos.2012.09.009.

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8

Baptiste, Virginie, Andréa Tommasi, Alain Vauchez, Sylvie Demouchy, and Roberta L. Rudnick. "Deformation, hydration, and anisotropy of the lithospheric mantle in an active rift: Constraints from mantle xenoliths from the North Tanzanian Divergence of the East African Rift." Tectonophysics 639 (January 2015): 34–55. http://dx.doi.org/10.1016/j.tecto.2014.11.011.

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9

Clutier, A., S. Gautier, and C. Tiberi. "Hybrid local and teleseismic P-wave tomography in North Tanzania: role of inherited structures and magmatism on continental rifting." Geophysical Journal International 224, no. 3 (2020): 1588–606. http://dx.doi.org/10.1093/gji/ggaa538.

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SUMMARY While local earthquake tomography is typically used to image the crust, this technique has restricted depth penetration due to short receiver-source distances. Regional tomography however aims to image the upper mantle from teleseismic events but suffers from poor resolution from 0 down to 40 km depth. We present here a hybrid method that combines the two approaches taking advantage of the short-wavelength resolution within the crust to better constrain the ray path at depth, and thus to improve the lithospheric imaging. Using this new method enhances the continuity or disruption of ma
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10

Tiberi, C., S. Gautier, C. Ebinger, et al. "Lithospheric modification by extension and magmatism at the craton-orogenic boundary: North Tanzania Divergence, East Africa." Geophysical Journal International 216, no. 3 (2018): 1693–710. http://dx.doi.org/10.1093/gji/ggy521.

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Dissertations / Theses on the topic "North Tanzanian Divergence"

1

Gama, Remigius. "Structure et propagation d'un rift magmatique en bordure de craton : approche intégrée de la divergence Nord-Tanzanienne par analyse des populations de failles et du réseau de drainage." Thesis, Brest, 2018. http://www.theses.fr/2018BRES0047/document.

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Tout modèle cinématique appliqué à la propagation du rift sud kenyan (RSK) et à sa divergence vers l’ouest au nord de la Tanzanie (DNT) doit nécessairement intégrer la vallée axiale Magadi-Natron (études antérieures), mais aussi le bloc soulevé Oldoinyo Ogol (OOB) à l’ouest (ce travail). Notre étude, basée pour l'essentiel sur l'interprétation d'imagerie satellitale SRTM 30 m, nous permet (1) de préciser l'organisation morphostructurale de l'ensemble du RSK, (2) d'identifier 2 systèmes successifs de failles bordières, (3) d'affirmer le rôle majeur de celle d'Oldoinyo Ogol, (4) d'élaborer un mo
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