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Relevant bibliographies by topics / Cameroon Volcanic Line

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Academic literature on the topic 'Cameroon Volcanic Line'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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Journal articles on the topic "Cameroon Volcanic Line"

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Nemzoue, P. N. N., N. A. K. Keutchafo, and J. P. Tchouankoue. "GEOTHERMAL DEVELOPMENT IN CAMEROON." Revista de Engenharia Térmica 19, no. 1 (2020): 32. http://dx.doi.org/10.5380/reterm.v19i1.76428.

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Africa is currently experiencing a period of economic growth. Its population is growing rapidly and its economies grow and diversify. To be sustainable, such growth requires a large investment in the energy sector. In the case of Cameroon hydroelectric energy is the main source of electrical power whereas the analysis of the geological point of view shows that Cameroon is unique in west-northern of Africa for its active volcanic line (with the last eruption of Mount Cameroon that last erupted in 1999 and 2000) that is a favorable zone for the production of power from geothermal resources. The

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Ngounouno Yamgouot, Fadimatou, Isaac Bertrand Gbambie Mbowou, Ismaïla Ngounouno, Azizi Abdoul Youpoungam, Isaac Daama, and Bernard Déruelle. "Insight into geochemistry of basaltic rocks from Mt Cameroon and characterization of the mantle source." International Journal of Advanced Geosciences 6, no. 2 (2018): 151. http://dx.doi.org/10.14419/ijag.v6i1.10738.

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Alkaline volcanic activities occurred in the Mt Cameroon at the ocean-continent boundary of the Cameroon Line. It is characterized by a volcanic association of alkali basalts and hawaiites extruded during the late Miocene to Recent times. The major and trace element geochemistry of the Mt Cameroon are consistent with the fractional crystallization of olivine ± clinopyroxene ± plagioclase (± amphibole). Petrographical and mineralogical study reveals the presence of xenocryts (olivine, clinopyroxene and spinel) in Mt Cameroon basalts. Their composition are similar to xenoliths and rocks crystals

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Ubangoh, R. U., I. G. Pacca, J. B. Nyobe, J. Hell, and B. Ateba. "Petromagnetic characteristics of Cameroon Line volcanic rocks." Journal of Volcanology and Geothermal Research 142, no. 3-4 (2005): 225–41. http://dx.doi.org/10.1016/j.jvolgeores.2004.11.006.

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Aminatou, Fagny Mefire, Nkouandou Oumarou Faarouk, Temdjim Robert, et al. "New K–AR ages of tchabal mbabo alkaline volcano massif, Cameroon volcanic line and adamawa plateau (central Africa)." International Journal of Advanced Geosciences 4, no. 2 (2016): 62. http://dx.doi.org/10.14419/ijag.v4i2.6516.

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Tchabal Mbabo in Central Africa is a voluminous volcano massif composed of alkali lava series. K-Ar geochronology data obtained from three samples of basanite - trachyandesite composition defined at least two volcanic activities. The first at end Eocene (38.22 ± 0.80 Ma) and the second during Oligocene (28.88 ± 0.61 and 28.60 ± 0.60Ma). The distribution of different ages along the Cameroon Volcanic Line is difficult to council with any migration of magmatic activity, as previously suggested. The most realistic scenario for the formation of Cameroon Line is that the ascent of lavas has been fav

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Tabod, C. T., J. D. Fairhead, G. W. Stuart, B. Ateba, and N. Ntepe. "Seismicity of the Cameroon Volcanic Line, 1982–1990." Tectonophysics 212, no. 3-4 (1992): 303–20. http://dx.doi.org/10.1016/0040-1951(92)90297-j.

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Tanyileke, G. Z., M. Kusakabe, and W. C. Evans. "Chemical and isotopic characteristics of fluids along the Cameroon Volcanic Line, Cameroon." Journal of African Earth Sciences 22, no. 4 (1996): 433–41. http://dx.doi.org/10.1016/0899-5362(96)00025-5.

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Hlaváč, Peter, Petr Baňař, and Eric Bertrand Fokam. "Pselaphinae of the Cameroon Volcanic Line. Part 3. A new genus of Goniacerini (Coleoptera: Staphylinidae: Goniaceritae) from Mount Cameroon." Zootaxa 5323, no. 2 (2023): 255–67. https://doi.org/10.11646/zootaxa.5323.2.5.

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Hlaváč, Peter, Baňař, Petr, Fokam, Eric Bertrand (2023): Pselaphinae of the Cameroon Volcanic Line. Part 3. A new genus of Goniacerini (Coleoptera: Staphylinidae: Goniaceritae) from Mount Cameroon. Zootaxa 5323 (2): 255-267, DOI: 10.11646/zootaxa.5323.2.5, URL: http://dx.doi.org/10.11646/zootaxa.5323.2.5

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Fagny, A. M., O. F. Nkouandou, J. M. Bardintzeff, et al. "Petrology and geochemistry of the Tchabal Mbabo volcano in Cameroon volcanic line (Cameroon, Central Africa): An intra-continental alkaline volcanism." Journal of African Earth Sciences 170 (October 2020): 103832. http://dx.doi.org/10.1016/j.jafrearsci.2020.103832.

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Milelli, L., L. Fourel, and C. Jaupart. "A lithospheric instability origin for the Cameroon Volcanic Line." Earth and Planetary Science Letters 335-336 (June 2012): 80–87. http://dx.doi.org/10.1016/j.epsl.2012.04.028.

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Hlaváč, Peter, and Petr Baňař. "Pselaphinae of the Cameroon Volcanic Line. Part 1. New Pselaphinae (Coleoptera, Staphylinidae) from the island São Tomé." Zootaxa 5222, no. 3 (2022): 267–76. https://doi.org/10.11646/zootaxa.5222.3.4.

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Hlaváč, Peter, Baňař, Petr (2022): Pselaphinae of the Cameroon Volcanic Line. Part 1. New Pselaphinae (Coleoptera, Staphylinidae) from the island São Tomé. Zootaxa 5222 (3): 267-276, DOI: 10.11646/zootaxa.5222.3.4

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Dissertations / Theses on the topic "Cameroon Volcanic Line"

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Tabod, Tabod Charles. "Seismological studies of the Cameroon Volcanic Line, in West Africa." Thesis, University of Leeds, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.305583.

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Nnange, Joseph Metuk. "The crustal structure of the Cameroon Volcanic Line and the Foumban Shear Zone based on gravity and aeromagnetic data." Thesis, University of Leeds, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.305782.

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Tambe-Ebot, Mathias Ashu Tako. "Proposing a Theoretical GIS Model for Landslides Analysis : The Case of Mount Cameroon." Thesis, Linköpings universitet, Institutionen för datavetenskap, 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-65899.

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This study presents a theoretical GIS model to investigate the relative impacts of geomorphic and environmental factors that govern the occurrence of landslides on the slopes of Mount Cameroon and its surrounding areas. The study area is located along the Cameroon Volcanic Line (CVL), a major structural feature that originates from the south Atlantic and continues into the continental landmass. The quite frequent seismic activity, geologic character, humid tropical climate and high human pressure on hill slopes are the major factors behind the occurrence of landslides in Mount Cameroon. This p

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Audhkhasi, Pranav. "Upper Crustal and Lithosphere-Asthenosphere Boundary Seismic Structure of 0-75 Ma old Normal Oceanic Lithosphere in the Equatorial Atlantic Ocean." Thesis, Université de Paris (2019-....), 2020. http://www.theses.fr/2020UNIP7056.

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Les études antérieures sur la croûte océanique supérieure se sont limitées à la jeune lithosphère et aux données sismiques à grand angle, qui manquent de résolution dans la croûte supérieure. La limite océanique lithosphère-asthénosphère (LAB) a été largement étudiée par des études sismologiques, mais souffre également d'une faible résolution verticale. L'expérience TransAtlantic ILAB a collecté des données de réflexion sismique multicanaux sur la lithosphère océanique âgée de 0 à 75 Ma formée sur la dorsale médio-atlantique à propagation lente dans l'océan Atlantique équatorial. L'analyse de

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Nkono, Collin. "Analyse multi-échelle et interprétation géodynamique des données morphostructurales associées au volcano-plutonisme phanérozoïque d'Afrique équatoriale (ligne du Caméroun et régions voisines)." Doctoral thesis, Universite Libre de Bruxelles, 2008. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/210440.

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De l’observation microscopique d’une lame mince à l’observation mégascopique d’une province volcano-plutonique par télédétection (SRTM, Landsat), ce travail s’intéresse aux méthodes de comptage, aux traitements statistique et fractale des tailles, formes, orientations et distributions spatiales ainsi qu’à l’interprétation pétrogénétique et/ou géodynamique de différents marqueurs géologiques (cristaux, linéaments, cônes volcaniques…) associés au volcano-plutonisme phanérozoïque d’Afrique équatoriale (Ligne du Cameroun et régions voisines).<p><p>L’analyse à l’échelle microscopique de la distribu

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Rankenburg, Kai [Verfasser]. "Megacrysts in volcanic rocks of the Cameroon volcanic line : constraints on magma genesis and contamination / von Kai Rankenburg." 2006. http://d-nb.info/978130359/34.

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Afungang, Roland Ngwatung. "Spacio-temporal probabilistic assessment of landslide hazard along the Bamenda Mountain Region of the Cameroon volcanic line." Doctoral thesis, 2015. https://repositorio-aberto.up.pt/handle/10216/79667.

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Afungang, Roland Ngwatung. "Spacio-temporal probabilistic assessment of landslide hazard along the Bamenda Mountain Region of the Cameroon volcanic line." Tese, 2015. https://repositorio-aberto.up.pt/handle/10216/79667.

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Book chapters on the topic "Cameroon Volcanic Line"

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Tefogoum, Ghislain Zangmo, Merlin Gountié Dedzo, Hyacinthe Zouyane Nouhou Dama, Raoul Merlin Ndonbou, Armand Kagou Dongmo, and David Guimolaire Nkouathio. "Mount Bambouto slopes geomorphosites (Cameroon Volcanic Line)." In GeoTourism for Social Sustainability and Ecological Justice in Sub-Saharan Africa. Routledge, 2024. http://dx.doi.org/10.4324/9781032706764-7.

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Ceríaco, Luis M. P., Bruna S. Santos, Ricardo F. de Lima, Rayna C. Bell, Sietze J. Norder, and Martim Melo. "Physical Geography of the Gulf of Guinea Oceanic Islands." In Biodiversity of the Gulf of Guinea Oceanic Islands. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-06153-0_2.

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AbstractThe Gulf of Guinea, in the Atlantic coast of Central Africa, has three oceanic islands that arose as part of the Cameroon Volcanic Line. From northeast to southwest these are Príncipe (139 km2), São Tomé (857 km2), and Annobón (17 km2). Although relatively close to the adjacent mainland, the islands have distinct climactic and geomorphologic characteristics, and have remained isolated throughout their geological history. Consequently, they have developed a unique biodiversity, rich in endemic species. We provide an integrated overview of the physical setting of the islands, including t

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Mendes, Luís F., and António Bivar-de-Sousa. "Butterflies and Skippers (Lepidoptera: Papilionoidea) of the Gulf of Guinea Oceanic Islands." In Biodiversity of the Gulf of Guinea Oceanic Islands. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-06153-0_13.

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AbstractThe three Gulf of Guinea oceanic islands, Príncipe, São Tomé, and Annobón, have always remained isolated from the African continent and correspond to the westernmost peaks of the Cameroon Volcanic Line, while the island of Bioko, part of the same ridge, was connected to the mainland during glaciations. Despite the small area of the oceanic islands, their relief and remoteness have enabled the evolution of remarkable ecological and biological diversity. Concerning diurnal Lepidoptera, 91 species and subspecies are known from the oceanic islands: 46 from Príncipe, 64 from São Tomé, and 8

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Zangmo, G. T., A. D. Kagou, D. G. Nkouathio, P. Wandji, and M. D. Gounté. "Geomorphological Features of the Manengouba Volcano (Cameroon Line): Assets for Geotourism and Other Anthropogenic Activities." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-10708-0_13.

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Teitchou, M. I., M. Grégoire, R. Temdjim, R. T. Ghogomu, C. Ngwa, and F. T. Aka. "Mineralogical and geochemical fingerprints of mantle metasomatism beneath Nyos volcano (Cameroon volcanic line)." In Geological Society of America Special Papers. Geological Society of America, 2011. http://dx.doi.org/10.1130/2011.2478(10).

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Nama, E. E. "Modelling variables to predict landslides in the south west flank of the Cameroon volcanic line, Cameroon, West Africa." In Unsaturated Soils for Asia. CRC Press, 2020. http://dx.doi.org/10.1201/9781003078616-145.

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Meguedong Guedia, Ange Merveille, Dieudonne Bisso, and Lionel Mbida Yem. "Geothermal Potential Assessment of the Bare-Bakem Region (Cameroon Volcanic Line): Contributions From Geophysical and Geothermometric Studies." In Chronicle of Computing. Oklahoma International Publishing, 2024. http://dx.doi.org/10.55432/978-1-6692-0005-5_8.

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In order to determine the geothermal potential of the municipality of Baré-Bakem, located in both the sedimentary basin of Moungo and the volcanic region of Nkongsamba (Cameroon Volcanic Line), geophysical measurements using electrical resistivity tomography were conducted along a 1km profile between two opposing thermal sources spaced 20 meters apart. The profile was acquired in the SW-NE direction using a 945m-long array with 64 electrodes spaced at 15 meters intervals. The ZZRes2Dinv44 software was employed to generate investigative images. The obtained results along the profile reveal the

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"Pyroclastic Rocks as Natural Fertilizer: Case Study of Volcanic Ashes from Tombel Graben (Cameroon Volcanic Line, Central Africa)." In Geotherapy. CRC Press, 2014. http://dx.doi.org/10.1201/b13788-32.

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"Rock Fertilizers as an Alternative to Conventional Fertilizers: The Use of Basalt from the Cameroon Volcanic Line for Maize Farming on Ferralitic Soils." In Geotherapy. CRC Press, 2014. http://dx.doi.org/10.1201/b13788-34.

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Conference papers on the topic "Cameroon Volcanic Line"

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Buian, Andrea. "PETROLOGY OF ULTRAMAFIC XENOLITHS AND HOST LAVAS OF NGAOUNDÉRÉ (ADAMAWA PLATEAU, CAMEROON VOLCANIC LINE)." In Cordilleran Section - 119th Annual Meeting - 2023. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023cd-387560.

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Marie Louise Vohnyui, Chenyi, Wotchoko Pierre, and Nkouathio David. "Volcanological and Petrological study of volcanic rocks from the North West flank of Oku volcanic complex (Cameroon volcanic line): Constraints from Mineralogy and Geochemistry." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.8764.

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Schmidt, Christoph, Tom Richter, and Lena Bullmann. "DOES THE MORPHOMETRY OF SCORIA CONES RELATE TO THEIR AGE? RESULTS FROM THE CAMEROON VOLCANIC LINE." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320687.

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Njome, M. S., C. E. Suh, and M. J. de Wit. "The Mount Cameroon Volcano, West Africa: an Active Link Between Recent Eruptives and Mantle Signatures of the Deep Past Beneath the Margins of Africa." In 11th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.241.njome_paper.

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