Lithospheric structure beneath the Central Africa Orogenic Belt in Cameroon from the analysis of satellite gravity and passive seismic data

• Published in: Tectonophysics 2018-10, Vol.745, p.326-337
• Main Authors: Goussi Ngalamo, Jeannot F., Sobh, Mohamed, Bisso, Dieudonne, Abdelsalam, Mohamed G., Atekwana, Estella, Ekodeck, Georges E.
• Format: Article
• Language: English
• Subjects: Assembly; Asthenosphere; Cenozoic; Central African Orogenic Belt; Channeling; Channelization; Cratons; Deformation; Domains; Geological history; Gravitation; Gravity; Gravity data; Lithosphere; Lithospheric structures; Mantle; Mathematical models; Mesozoic; Modelling; Moho; Orogeny; Passive seismic data; Plate tectonics; Plateaus; Power spectral analysis; Precambrian; Satellite gravity data; Satellite systems; Satellites; Seismic data; Seismic surveys; Seismological data; Seismology; Spectral analysis; Spectrum analysis; Superposition (mathematics); Thermal analysis; Thermal models; Two dimensional analysis; Uplift
• ISSN: 0040-1951; 1879-3266
• DOI: 10.1016/j.tecto.2018.08.015

We present original results that contribute to the understanding of lithospheric structures modification of regions that have witnessed superimposition of multiple tectonic events throughout their geological history. We analyze satellite gravity data through two-dimensional radially-averaged power spectral analysis as well as passive seismic data through thermal modeling to image the depth to the Moho and the lithosphere - asthenosphere boundary (LAB beneath the Central Africa Orogenic Belt (CAOB). The CAOB is an ENE-trending deformation belt extending from Cameroon in the west to Sudan in the east. In Cameroon, it is found on the northern edge of the Congo craton represented by the Oubanguides orogenic belt (the Western Cameroon, the Adamawa – Yade, and the Yaoundé domains). It coincides with the Adamawa plateau and the Benue Trough, and it is spotted by the Cenozoic Cameroon Volcanic Line (CVL). The CAOB was formed during the Precambrian Greater Gondwana assembly but was reactivated during the Mesozoic as a result of Gondwana breakup. We find deeper Moho and LAB) beneath Congo craton and the Yaoundé domain reaching ~50 km and ~200 km, respectively. We map shallower Moho and LAB beneath the CAOB (together with the Adamawa plateau and the Benue trough) reaching ~25 km and ~70 km, respectively. We interpret the shallower LAB beneath the CAOB as due to zonal sub-continental lithospheric mantle (SCLM) delamination along the northern edge of the Congo craton that occurred in association with collisional assembly of Greater Gondwana. This allowed for channelization of mantle flow during the Cenozoic resulting in the formation of the CVL and the uplift of the Adamawa plateau. Our approach can be used to understand the modification of lithospheric structures beneath other terrains that have long tectonic history. [Display omitted] •Thinner lithosphere underlies the Central African Orogenic Belt in Cameroon.•Thinner lithosphere beneath the orogenic belt is caused by mantle delamination.•Mantle flow guided by thinner lithosphere formed the Cameroon Volcanic Line.