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Boris Chako Tchamabé

Researcher at Tokai University

Publications -  12
Citations -  212

Boris Chako Tchamabé is an academic researcher from Tokai University. The author has contributed to research in topics: Maar & Pyroclastic rock. The author has an hindex of 8, co-authored 11 publications receiving 139 citations. Previous affiliations of Boris Chako Tchamabé include University of Douala & National Autonomous University of Mexico.

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Journal ArticleDOI

A comparative review of petrogenetic processes beneath the Cameroon Volcanic Line: Geochemical constraints

TL;DR: The origin and petrogenesis of the Cameroon Volcanic Line (CVL), composed of volcanoes that form on both the ocean floor and the continental crust, are difficult to understand because of the diversity, heterogeneity, and nature of available data as mentioned in this paper.
Book ChapterDOI

How Polygenetic are Monogenetic Volcanoes: Case Studies of Some Complex Maar‐Diatreme Volcanoes

TL;DR: A maar-diatreme volcano is recognized by a volcanic crater that is cut into country rocks and surrounded by a low-height ejecta rim composed of pyroclastic deposits of few meters to up to 200 m thick above the surface level.
Journal ArticleDOI

Eruptive history of the Barombi Mbo Maar, Cameroon Volcanic Line, Central Africa: Constraints from volcanic facies analysis

TL;DR: The first and detail field investigations of exposed deposits at proximal sections of the Barombi Mbo Maar (BMM), NE Mt Cameroon, with the aim of documenting its past activity, providing insight on the stratigraphic distribution, depositional process, and evolution of the eruptive sequences during its formation as mentioned in this paper.
Journal ArticleDOI

Petrology and geochemistry of lavas from Gawar, Minawao and Zamay volcanoes of the northern segment of the Cameroon volcanic line (Central Africa): Constraints on mantle source and geochemical evolution

TL;DR: In this article, the authors present the case of the Gawar, Zamay and Minawao volcanoes, for which, for the first time, petrological and geochemical data comprising major and trace elements, and Strontium-Neodymium-Lead isotopes have been used to investigate the mantle source and the genetic relation between the felsic and mafic lavas in these areas.