Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Pierre Wandji"'
Autor:
Dieudonné Tchokona Seuwui, Hervé Bellon, Benoît Joseph Mbassa, Rose Noel Ngo Belnoun, Pierre Wandji, Pierre Wotchoko, Jacques-Marie Bardintzeff, Sébastien Owona, Zénon Itiga
Publikováno v:
Journal of Geosciences and Geomatics. 9:160-176
The Cretaceous Ngaou Boh anorogenic complex (NBAC) located in the far North Adamawa Plateau, the centre domain of the Cameroon Line constitutes a plutonic-volcanic ring association. The whole rock K-Ar datation yields a crystallization age of ca. 74
Autor:
Benjamin Ntieche, Pauline Wokwenmendam Nguet, Dieudonne Charles Isidore Ilouga, Amidou Moundi, Mekala Ram Mohan, Mahomed Aziz Mounjouohou, Zakari Nchouwet, Pierre Wandji
Publikováno v:
Arabian Journal of Geosciences. 15
Autor:
Robert Temdjim, Caroline Neh Ngwa, Anicet Feudjio Tiabou, Pierre Wandji, Jacques-Marie Bardintzeff, Edith Ekatah Bate Tibang, François Xavier Onana Mebara, Vivian Bih Che
Publikováno v:
Acta Geochimica
Acta Geochimica, Springer, 2019, 38 (1), pp.40-67. ⟨10.1007/s11631-018-0272-9⟩
Acta Geochimica, Springer, 2019, 38 (1), pp.40-67. ⟨10.1007/s11631-018-0272-9⟩
International audience; Three monogenetic cones in the Baossi-Warack area, Ngaoundere, Adamawa Plateau forming part of the Cameroon Volcanic Line (CVL) are documented in this study. Basaltic lavas (
Autor:
Dieudonné Tchokona Seuwui, Bernard Bonin, Benoît Joseph Mbassa, Zénon Itiga, Rose Noel Ngo Belnoun, Ntepe Nfomou, Pierre Wandji, Jacques-Marie Bardintzeff, Pierre Wotchoko, Hervé Bellon
Publikováno v:
Journal of African Earth Sciences
Journal of African Earth Sciences, Elsevier, 2019, 149: (398-425), ⟨10.1016/j.jafrearsci.2018.08.019⟩
Journal of African Earth Sciences, Elsevier, 2019, 149: (398-425), ⟨10.1016/j.jafrearsci.2018.08.019⟩
International audience; In the Cameroon Pan-African orogenic belt, the West Cameroon Domain (WCD) is characterized by the apparent lack of Archean-Paleoproterozoic relicts, the development of Neoproterozoic basins and abundant plutonic massifs. The H
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cc82332609057ed3362c7f4ce1bf8dbc
https://hal.archives-ouvertes.fr/hal-01900960
https://hal.archives-ouvertes.fr/hal-01900960
Autor:
Armand Kagou Dongmo, David Guimolaire Nkouathio, Pulchérie Chakam Tagheu, Hervé Bellon, Jacques-Marie Bardintzeff, Gilles Ruffet, Pierre Wandji, André Pouclet
Publikováno v:
Journal of African Earth Sciences
Journal of African Earth Sciences, 2014, 97, pp.297-321. ⟨10.1016/j.jafrearsci.2014.04.023⟩
Journal of African Earth Sciences, Elsevier, 2014, 97, pp.297-321. ⟨10.1016/j.jafrearsci.2014.04.023⟩
Journal of African Earth Sciences, 2014, 97, pp.297-321. ⟨10.1016/j.jafrearsci.2014.04.023⟩
Journal of African Earth Sciences, Elsevier, 2014, 97, pp.297-321. ⟨10.1016/j.jafrearsci.2014.04.023⟩
International audience; The volcanic story of Mount Manengouba is related to four chronological stages: (1) forming of the early Manengouba shield volcano between 1.55 and 0.94 Ma, (2) building of the Eboga strato-cone between 0.94 and 0.89 Ma, (3) c
Autor:
Armand Kagou Dongmo, David Guimolaire Nkouathio, Ghislain Zangmo Tefogoum, Pierre Wandji, Merlin Gountié Dedzo
Publikováno v:
Geoheritage. 6:225-239
Mount Manengouba is a volcanic complex, age between 1.5 and 0 Myr, situated in the Cameroon Line in Cameroon, approximately 120 km NE of Mount Cameroon. It comprises some important geomorphological features, of geoheritage significance, i.e., geomorp
Publikováno v:
Arabian Journal of Geosciences. 7:4641-4664
Tchabal Gangdaba (TG) volcanic massif, which is a part of the continental sector of the Cameroon Volcanic Line (CVL), is dated between 34.4 and 25.1 Ma. It displays mafic lavas (picrobasalt and basanite, 41–43 wt % SiO2) and felsic lavas (rhyolite,
Autor:
Pierre Wotchoko, Gerald Ngnoupeck, Pierre Wandji, Christian Suh Guedjeo, Jacques-Marie Bardintzeff, Armand Kagou Dongmo, David Guimolaire Nkouathio, Zénon Itiga
Publikováno v:
Open Geosciences, Vol 8, Iss 1, Pp 429-449 (2016)
The Ndop Plain, located along the Cameroon Volcanic Line (CVL), is a volcano-tectonic plain, formed by a series of tectonic movements, volcanic eruptions and sedimentation phases. Floods (annually) and landslides (occasionally) occur with devastating
Publikováno v:
Acta Geologica Sinica - English Edition. 83:1008-1016
Mount Bambouto is a polygenic stratovolcano of the Cameroon Volcanic Line, built between 21 Ma and 4.5 Ma. It is situated approximately 200 km NE of Mount Cameroon, between 09° 55′ and 10°15′ longitude east and, 05°25′ and 05°50′ latitude
Autor:
Jacques-Marie Bardintzeff, Oumar Farouk Mouncherou, Hervé Bellon, Amidou Moundi, Jean-Jacques Ménard, Pierre Wandji, Eric Reusser, Félix M. Tchoua, Lise Carole Okomo Atouba
Publikováno v:
Comptes Rendus Geoscience. 339:396-406
Resume Les basaltes transitionnels eocenes occupent plus de la moitie ouest des affleurements laviques du plateau Bamoun. Les basaltes de ce type restent exceptionnels dans la ligne volcanique du Cameroun (LVC). Ils possedent des caracteristiques pet