Evolution of volcanism in graben and horst structures along the Cenozoic Cameroon Line (Africa): implications for tectonic evolution and mantle source composition
DG Nkouathio, A Kagou Dongmo, JM Bardintzeff… - Mineralogy and …, 2008 - Springer
Abstract Tombel graben and Mounts Bambouto are two volcanic fields of the typical system
of alternating graben and horst structure of the Cameroon Volcanic Line. Tombel graben is a …
of alternating graben and horst structure of the Cameroon Volcanic Line. Tombel graben is a …
Volcano-tectonics of the Al haruj volcanic province, Central Libya
Abstract The Al Haruj intra-continental Volcanic Province (AHVP), located at the south-
western margin of the Sirt Basin, hosts the most extensive and recent volcanic activity in …
western margin of the Sirt Basin, hosts the most extensive and recent volcanic activity in …
Plate kinematics and geodynamics in the Central Mediterranean
M Viti, E Mantovani, D Babbucci, C Tamburelli - Journal of Geodynamics, 2011 - Elsevier
We argue that seismotectonic activity in the Central Mediterranean area and the Aegean–
Balkan zone is driven by the NNE-ward motion of Africa and westward motion of Anatolia …
Balkan zone is driven by the NNE-ward motion of Africa and westward motion of Anatolia …
[HTML][HTML] The Kufrah paleodrainage system in Libya: A past connection to the Mediterranean Sea?
P Paillou, S Tooth, S Lopez - Comptes …, 2012 - comptes-rendus.academie-sciences …
Paillou et al.(2009) mapped a 900 km-long paleodrainage system in eastern Libya, the
Kufrah River, that could have linked the southern Kufrah Basin to the Mediterranean coast …
Kufrah River, that could have linked the southern Kufrah Basin to the Mediterranean coast …
Geologic and metallogenic framework of North Africa
M Bouabdellah, JF Slack - Mineral Deposits of North Africa, 2016 - Springer
North Africa is noteworthy for having a great diversity of geology and mineral resources.
Geologically, the region contains numerous terranes that contain rocks ranging in age from …
Geologically, the region contains numerous terranes that contain rocks ranging in age from …
Petrogenesis of Cenozoic volcanic rocks in the NW sector of the Gharyan volcanic field, Libya
The north-western sector of the Gharyan volcanic field (northern Libya) consists of trachytic-
phonolitic domes emplaced between~ 41 and 38Ma, and small-volume mafic alkaline …
phonolitic domes emplaced between~ 41 and 38Ma, and small-volume mafic alkaline …
Geochemistry of 24 Ma basalts from NE Egypt: source components and fractionation history
C Endress, T Furman, MAA El-Rus… - … Society, London, Special …, 2011 - lyellcollection.org
Subalkaline basalts from NE Egypt represent an episode of magmatism at c. 24 Ma,
coincident with widespread eruptive activity in northern Africa. New geochemical data …
coincident with widespread eruptive activity in northern Africa. New geochemical data …
Rift architecture and evolution: The Sirt Basin, Libya: The influence of basement fabrics and oblique tectonics
KM Abdunaser, KJW McCaffrey - Journal of African Earth Sciences, 2014 - Elsevier
Abstract The Cretaceous-Tertiary northwest-trending Sirt Basin system, Libya, is a rift/sag
basin formed on Pan-African to Paleozoic-aged basement of North Africa. In this study, we …
basin formed on Pan-African to Paleozoic-aged basement of North Africa. In this study, we …
Petrogenesis of the eastern part of the Al Haruj basalts (Libya)
The eastern part of the Al Haruj volcanic field (central Libya) is dominated by lava flows with
subordinate dykes as well as scoria and spatter cone deposits which formed around 4–0.5 …
subordinate dykes as well as scoria and spatter cone deposits which formed around 4–0.5 …
Miocene to recent alkaline volcanism between Al Haruj and Waw an Namous (southern Libya)
Unspiked K–Ar ages, petrological, geochemical and isotopic data are reported on samples
from southern Libya (Wan an Namous—Al Haruj area). The Wan an Namous intracaldera …
from southern Libya (Wan an Namous—Al Haruj area). The Wan an Namous intracaldera …