Subsurface structure and stratigraphy of the northwest end of the Turkana Basin, Northern Kenya Rift, as revealed by magnetotellurics and gravity joint inversion
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- 作者：Yassine Abdelfettaha ; b ; c ; yassine.abdelfettah@unistra.fr" class="auth_mail" title="E-mail the corresponding author ; Jean-Jacques Tiercelind ; riftman@orange.fr" class="auth_mail" title="E-mail the corresponding author ; Pascal Taritsb ; tarits@univ-brest.fr" class="auth_mail" title="E-mail the corresponding author ; Sophie Hautote ; sophie.hautot@imagir.eu" class="auth_mail" title="E-mail the corresponding author ; Marcia Maiab ; marcia@univ-brest.fr" class="auth_mail" title="E-mail the corresponding author ; Peter Thuof ; b ; pthuo@erhc.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Northern Kenya Rift ; Turkana Basin ; Kachoda Basin ; Lapur Sandstone ; &ldquo ; Turkana Volcanics&rdquo ; Sub-basalt imaging ; Magnetotelluric ; Gravity ; Joint inversion
- 刊名：Journal of African Earth Sciences
- 出版年：2016
- 出版时间：July 2016
- 年：2016
- 卷：119
- 期：Complete
- 页码：120-138
- 全文大小：9917 K
文摘
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Confirm the Turkana half-graben basins geometry and organization at depth.
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Delineate the “Turkana Volcanics” unit as well as horizontal/vertical variations.
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Characterize the depth and topography of the basement in the Northwest Turkana and Kachoda basins.
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Characterization of the new Kachoda half-graben basin from geometries to stratigraphy.
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MT and gravity data used in Turkana to surpass the poor quality of seismic.