Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Alembert Alexandre Ganwa"'
Autor:
Sylvestre Ganno, Gentry C. Fuh, Tessontsap Teutsong, Gaelle S. N. Assomo, Paul-Désiré Ndjigui, Alembert Alexandre Ganwa
Publikováno v:
Geosciences Journal. 26:55-78
Ngaye area belongs to the Adamawa-Yade domain (AYD) of the Central African Fold Belt (CAFB) in Cameroon. It is underlain by gneisses and amphibolites intruded by a variety of granitoids including granites and granodiorites. Petrographic, mineralogica
Autor:
Gaelle Sandra Assomo Ngono, Paul-Désiré Ndjigui, Sylvestre Martial Ntomba, Alembert Alexandre Ganwa
Publikováno v:
Geological Journal. 56:5176-5198
Publikováno v:
Geological Journal. 53:2955-2968
Autor:
Depesquidoux Tchaptchet Tchato, Alembert Alexandre Ganwa, Jean Pierre Tchouankoue, Rose Noel Ngo Belnoun, Nicole Armelle Wambo Simeni
Publikováno v:
International Journal of Geosciences. :318-331
The work is a vivid description of the structural relationship between brittle deformation of the Precambrian basement in the southern continental part of the Cameroon Line and intrusive Paleozoic and Mesozoic basalt dykes swarms. A multidisciplinary
Publikováno v:
Journal of African Earth Sciences. 120:12-22
The main geological feature of Central Cameroon is the wide spread occurrence of granitoids emplaced in close association with transcurrent regional shear zones. The basement of this vast domain is a Paleoproterozoic ortho-and para-derivative formati
Autor:
Oumar Mahamat, Oumarou F. Nkouandou, Alembert Alexandre Ganwa, Jacques-Marie Bardintzeff, Aminatou Fagny Mefire
Publikováno v:
Open Geosciences, Vol 9, Iss 1, Pp 138-150 (2017)
Dolerite dykes are widespread in the Mongo area within the granitic Guéra Massif (Chad, Central Africa). Dykes are several hundred metres to several kilometres long, a metre to decametre thick, and vertical, crosscutting the Pan-African granitic bas
Publikováno v:
Australian Journal of Earth Sciences. 60:649-658
The northwestern part of southwest Chad is one of the best regions to find exposed Precambrian terrains and their Phanerozoic cover. In this area, it is easy to establish the lithostratigraphic and structural relationships between sedimentary and gra
Publikováno v:
International Geology Review. 53:759-784
The Meiganga area is situated in the Adamawa–Yade domain (AYD) of the Pan-African fold belt in Cameroon. The AYD is characterized by abundant plutonic rocks that intruded Palaeoproterozoic gneisses. It is cut by the transcurrent Central Cameroonian
Autor:
C. K. Shang, Alembert Alexandre Ganwa, Wolfgang Siebel, Jacqueline Tchakounte Numbem, Joseph Mvondo Ondoa, Wolfgang Frisch, Muharrem Satir
Publikováno v:
Journal of African Earth Sciences. 51:77-88
The Kombe-II area belongs to the southern part of the Cameroonian Panafrican belt. It is made up of different gneisses, amphibolites and quartzites of the Bafia Group. This volcano-sedimentary rock sequence became polyphasely deformed and metamorphos
Autor:
Vincent Ngako, Wolfgang Frisch, Wolfgang Siebel, Georges Emmanuel Ekodeck, Alembert Alexandre Ganwa, Cosmas K. Shang
Publikováno v:
Comptes Rendus Geoscience. 340:211-222
The Meiganga area is located in the central part of the Panafrican belt of Cameroon. This region is underlain by a granitic and gneissic basement, crosscut, and covered by basaltic and phonolitic rocks. To the southwest of Meiganga, the pyroxene-anda