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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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 Abdelfettah^a ; ^b ; ^c ; ^{yassine.abdelfettah@unistra.fr" class="auth_mail" title="E-mail the corresponding author} ; Jean-Jacques Tiercelin^d ; ^{riftman@orange.fr" class="auth_mail" title="E-mail the corresponding author} ; Pascal Tarits^b ; ^{tarits@univ-brest.fr" class="auth_mail" title="E-mail the corresponding author} ; Sophie Hautot^e ; ^{sophie.hautot@imagir.eu" class="auth_mail" title="E-mail the corresponding author} ; Marcia Maia^b ; ^{marcia@univ-brest.fr" class="auth_mail" title="E-mail the corresponding author} ; Peter Thuo^f ; ^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

•: Confirm the Turkana half-graben basins geometry and organization at depth.
•: Delineate the “Turkana Volcanics” unit as well as horizontal/vertical variations.
•: Characterize the depth and topography of the basement in the Northwest Turkana and Kachoda basins.
•: Characterization of the new Kachoda half-graben basin from geometries to stratigraphy.
•: MT and gravity data used in Turkana to surpass the poor quality of seismic.