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Dive into the research topics where Pierre Wandji is active.

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Featured researches published by Pierre Wandji.


Journal of African Earth Sciences | 2002

The Tombel graben (West Cameroon): a recent monogenetic volcanic field of the Cameroon Line

D. G. Nkouathio; Jean-Jacques Ménard; Pierre Wandji; Jacques-Marie Bardintzeff

The Tombel graben is a recent monogenetic volcanic field located in the continental part of the Cameroon Line. Magmatic activity began with fissure eruptions emitting large lava flows, and continued with explosive episodes generating cinder cones. Tombel lava flows are made up of three major rock types. Ankaramite yields phenocrysts of Fe–Ti oxides, forsterite olivine and diopside-augite clinopyroxene. In addition to this assemblage, basalt and hawaiite (olivine basalt, doleritic basalt and trachybasalt according to their modal compositions) contain phenocrysts of labradorite-andesine plagioclase and scarce kaersutite. The suite of lava flows, ranging from ankaramite to hawaiite, define an incomplete sodic alkaline series. Moreover, basanite, rich in incompatible elements, is locally found as late ejecta. Geochemical data share some oceanic island basalt (OIB) characteristics. It is suggested that the ankaramite–hawaiite series could be due to differing degrees of partial melting of a source at the asthenosphere–lithosphere boundary, followed by low rates of fractional crystallization.


Open Geosciences | 2016

Geohazards (floods and landslides) in the Ndop plain, Cameroon volcanic line

Pierre Wotchoko; Jacques-Marie Bardintzeff; Zénon Itiga; D. G. Nkouathio; Christian Suh Guedjeo; Gerald Ngnoupeck; Armand Kagou Dongmo; Pierre Wandji

Abstract 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 environmental effects. However, this plain attracts a lot of inhabitants owing to its fertile alluvial soils. With demographic explosion in the plain, the inhabitants (143,000 people) tend to farm and inhabit new zones which are prone to these geohazards. In this paper, we use field observations, laboratory analyses, satellite imagery and complementary methods using appropriate software to establish hazard (flood and landslide) maps of the Ndop Plain. Natural factors as well as anthropogenic factors are considered. The hazard maps revealed that 25% of the area is exposed to flood hazard (13% exposed to high flood hazard, 12% to moderate) and 5% of the area is exposed to landslide hazard (2% exposed to high landslide hazard, 3% to moderate). Some mitigation measures for floods (building of artificial levees, raising foundations of buildings and the meticulous regulation of the flood guards at Bamendjing Dam) and landslides (slope terracing, planting of trees, and building retaining walls) are proposed.


Mineralogy and Petrology | 2008

Evolution of volcanism in graben and horst structures along the Cenozoic Cameroon Line (Africa): implications for tectonic evolution and mantle source composition

D. G. Nkouathio; A. Kagou Dongmo; Jacques-Marie Bardintzeff; Pierre Wandji; Hervé Bellon; André Pouclet


Comptes Rendus Geoscience | 2007

Les basaltes éocènes à affinité transitionnelle du plateau Bamoun, témoins d’un réservoir mantellique enrichi sous la ligne volcanique du Cameroun

Amidou Moundi; Pierre Wandji; Jacques-Marie Bardintzeff; Jean-Jacques Ménard; Lise Carole Okomo Atouba; Oumar Farouk Mouncherou; Éric Reusser; Hervé Bellon; Félix M. Tchoua


Mineralogy and Petrology | 2009

Xenoliths of dunites, wehrlites and clinopyroxenites in the basanites from Batoke volcanic cone (Mount Cameroon, Central Africa): petrogenetic implications

Pierre Wandji; J. P. F. Tsafack; Jacques-Marie Bardintzeff; D. G. Nkouathio; A. Kagou Dongmo; Hervé Bellon; Hervé Guillou


Journal of African Earth Sciences | 2010

The discovery of late Quaternary basalt on Mount Bambouto: Implications for recent widespread volcanic activity in the southern Cameroon Line

Armand Kagou Dongmo; D. G. Nkouathio; André Pouclet; Jacques-Marie Bardintzeff; Pierre Wandji; Alexandre Nono; Hervé Guillou


Comptes Rendus De L Academie Des Sciences Serie Ii Fascicule A-sciences De La Terre Et Des Planetes | 2000

Éruptions simultanées de basalte alcalin et de hawaiite au mont Cameroun (28 mars-17 avril 1999)

Bernard Déruelle; Jacques-Marie Bardintzeff; Jean-Louis Cheminée; Ismaïla Ngounouno; Justin Lissom; Charles Nkoumbou; Jacques Etame; Joseph-Victor Hell; Gregory Tanyileke; Jean N'ni; Bekoa Ateba; Ntomu Ntepe; Alexandre Nono; Pierre Wandji; Jacob Fosso; David G Nkouathio


Comptes Rendus De L Academie Des Sciences Serie Ii Fascicule A-sciences De La Terre Et Des Planetes | 2001

Évolution volcanologique du mont Manengouba (Ligne du Cameroun) ; nouvelles données pétrographiques, géochimiques et géochronologiques

Armand Kagou Dongmo; Pierre Wandji; André Pouclet; Jean-Paul Vicat; Alain Cheilletz; David Guimolaire Nkouathio; Pavel Alexandrov; Félix M. Tchoua


Mineralogy and Petrology | 2008

Rhyolites of the Mbépit Massif in the Cameroon Volcanic Line: an early extrusive volcanic episode of Eocene age

Pierre Wandji; Dieudonné Tchokona Seuwui; Jacques-Marie Bardintzeff; Hervé Bellon; Bernard Platevoet


Géochronique | 2003

La ligne du Cameroun : volcanologie et géochronologie de trois régions (Mont Manengouba, Plaine du Noun et Tchabal Gangdaba).

Z. Itiga; P.-J. Chakam Tagheu; P. Wotchoko; Pierre Wandji; Jacques-Marie Bardintzeff; Hervé Bellon

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Hervé Bellon

Centre national de la recherche scientifique

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Amidou Moundi

University of Yaoundé I

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