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Spatial distribution and alignments of volcanic centers: clues to the formation of monogenetic volcanic fields
Monogenetic basaltic volcanic fields occur worldwide in tectonic environments ranging from
extensional to convergent. Understanding similarities and differences between these fields …
extensional to convergent. Understanding similarities and differences between these fields …
Evolution and characteristics of continental rifting: Analog modeling-inspired view and comparison with examples from the East African Rift System
The evolution and characteristics of narrow continental rifting are illustrated in this paper
through a review of recent lithospheric-scale analog models of continental extension …
through a review of recent lithospheric-scale analog models of continental extension …
Lateral magma flow in mafic sill complexes
The structure of upper crustal magma plumbing systems controls the distribution of
volcanism and influences tectonic processes. However, delineating the structure and …
volcanism and influences tectonic processes. However, delineating the structure and …
The Cenozoic magmatism of East Africa: part V–magma sources and processes in the East African Rift
The generation of magmas in the East African Rift System (EARS) is largely the result of
either:(A) melting of easily fusible compositions located within the lithospheric mantle due to …
either:(A) melting of easily fusible compositions located within the lithospheric mantle due to …
Volcanic activity and hazard in the East African Rift Zone
Over the past two decades, multidisciplinary studies have unearthed a rich history of
volcanic activity and unrest in the densely-populated East African Rift System, providing new …
volcanic activity and unrest in the densely-populated East African Rift System, providing new …
Quantifying volcanic hazard at Campi Flegrei caldera (Italy) with uncertainty assessment: 1. Vent opening maps
Campi Flegrei is an active volcanic area situated in the Campanian Plain (Italy) and
dominated by a resurgent caldera. The great majority of past eruptions have been explosive …
dominated by a resurgent caldera. The great majority of past eruptions have been explosive …
Elevated mantle temperature beneath East Africa
The causes of magmatism at magmatic rifted margins and large igneous provinces (LIPs)
are uncertain because the condition of the mantle that underlay them during formation can …
are uncertain because the condition of the mantle that underlay them during formation can …
Off-rift volcanism in rift zones determined by crustal unloading
When continents are stretched over a long period of time, deep elongated rift valleys form at
Earth's surface and zones of ponded magma, centred beneath the rift, form at the crust …
Earth's surface and zones of ponded magma, centred beneath the rift, form at the crust …
Crustal structure of active deformation zones in Africa: Implications for global crustal processes
Abstract The Cenozoic East African rift (EAR), Cameroon Volcanic Line (CVL), and Atlas
Mountains formed on the slow‐moving African continent, which last experienced orogeny …
Mountains formed on the slow‐moving African continent, which last experienced orogeny …
The control of preexisting faults on the distribution, morphology, and volume of monogenetic volcanism in the Michoacán-Guanajuato Volcanic Field
Interactions between volcanic and tectonic processes affect the distribution, morphology,
and volume of eruptive products in space and time. The Queréndaro area in the eastern …
and volume of eruptive products in space and time. The Queréndaro area in the eastern …