Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Amidou MOUNDI"'
Publikováno v:
International Journal of Geoheritage and Parks, Vol 11, Iss 3, Pp 464-482 (2023)
This study was carried out in the Foumbot-Kouomboum region (Noun Plain, Cameroon Volcanic Line), with the main objective of presenting (i) the geomorphological characteristics of the volcanic landforms and (ii) the inventory and evaluation of the mai
Externí odkaz:
https://doaj.org/article/58ec2528b64b48258d862cfe667fb5b4
Autor:
Luc Achille Ziem A Bidias, Sahada Mouchili Nguegni, Dieudonné Charles Isidore Ilouga, Hermine Suzinie Kenna, Amidou Moundi, Pierre Kamgang
Publikováno v:
International Journal of Geoheritage and Parks, Vol 11, Iss 3, Pp 365-384 (2023)
This study was conducted in Kouoptamo, located in the Noun Plain in Western Cameroon, with the main objective of inventorying and evaluating the geological heritage, and promoting the protection and geoconservation of geosites, and their use in geoto
Externí odkaz:
https://doaj.org/article/00dbb13e3b2a415e898dc048e16f58f0
Publikováno v:
Geosystems and Geoenvironment, Vol 2, Iss 4, Pp 100213- (2023)
This study presents petrography, mineral chemistry, whole-rock major and trace elemental systematics for Recent pyroclastic deposits from volcanic edifices of Baïgom and Petpenoun, located in the Noun Plain graben along the Cameroon Volcanic Line (C
Externí odkaz:
https://doaj.org/article/a0e5d133c05d45968c1b1338e85604a7
Autor:
Oumar Farouk MOUNCHEROU, Amidou MOUNDI, Olivier NJIKEU, Aicha FOUPOUAGNIGNI, Zakari MFONKA, Oumar Farikou MFOCHIVE, Jean Claude TONGA, Jules Remy Ndam NGOUPAYOU, Appolinaire TAGNE
Publikováno v:
Journal of Water and Environmental Sciences, Vol 2, Iss 2, Pp 359-379 (2018)
The Noun volcanic plain is a southern west entity of the Bamoun Plateau which was the site of various volcanic episodes. Aquifers distribution in this environment constitutes the principal water source of the area, intended to human consumption and a
Externí odkaz:
https://doaj.org/article/6671aba2b4124be6817ad2e0bce27ea2
Autor:
Benjamin Ntieche, Pauline Wokwenmendam Nguet, Amidou Moundi, Ram Mohan Mekala, Mahomed Aziz Mounjouohou, Chimene Grace Staelle Atsalang, Zakari Nchouwet
Publikováno v:
International Journal of Earth Sciences. 111:1223-1250
Autor:
Benjamin Ntieche, Wokwenmendam Nguet Pauline, Eric José Messi Ottou, Mahomed Aziz Mounjouohou, Zakari Nchouwet, Minamou Guy Bertin, Daouda Mfepat, Amidou Moundi
Publikováno v:
Earth Sciences Pakistan. 6:07-16
Field and petrographic studies of the Makenene area in the Central African Fold Belt in Cameroon reveals several features testifying the mafic and felsic magmas interactions and their coeval nature. They are: (1) the Mafic Magmatic Enclaves (MMEs) sc
Autor:
Amidou Moundi, Mohammad Bello, Yvette Frida Danwe, Jules Remy Ndam Ngoupayou, Zakari Mfonka, Oumarou Farikou Mfochive, Amidou Kpoumié, Olivier Njikeu, Jean Claude Tonga, Brice Tchakam Kamtchueng, Oumar Farouk Mouncherou
Publikováno v:
Journal of Water Resource and Protection. 11:558-576
The problem of groundwater supply in the Bamun plateau situated in the Cameroon Volcanic Line exists and no proper solution has been found so far. This investigation intends to find the suitable groundwater potential zones by overlaying the geomorpho
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
Publikováno v:
Journal of Geoscience and Environment Protection. :195-209
Pyroclastics which are known natural pozzolanic materials due to amorphous contents, are present in several areas of the Mbepit Massif in West Cameroon. In this work natural pozzolan from three zones namely Pouoloum, Njimbouot and Nkouonja were chara
Autor:
Mahomed Aziz Mounjouohou, Amidou Moundi, Zakari Nchouwet, Benjamin Ntieche, Daouda Mfepat, M. Ram Mohan, Pauline Wokwenmendam Nguet
Publikováno v:
SN Applied Sciences. 3
The Tikar plain is located on the Cameroon Central Shear Zone. It is also part of the North Equatorial Pan-African Belt. It is formed of granitoids intruded in places by mafic and intermediate dykes. The mafic dykes are essentially banded gabbros com