10 research outputs found
Textures in mylonitised granite from Banefo area in the central part of the Cameroon Central Shear Zone (central Africa) — Kinematics and gradian deformation indicators
The North Equatorial Panafrican belt
is constituted by orthogneissified metamorphic
and magmatic sets linked to
tectonometamorphic events of the neoproterozoic
orogeny. This belt whose
formations are situated in the North of
the congo craton is divided into three
distinct geodynamic domains: a southern
domain, a northern domain and a
central domain. The deformation and
metamorphism relationships are a function
of the different geodynamic domains
of the belt.
The central domains, to which belongs
the Banefo region, is affected by large
strike-slip faults among which is the central
cameroonian shear zone. This domain
is marked out by numerous syntectonic
granitoids. At Banefo (NE
Bafoussam, West Cameroon), those
massifs are mainly constituted by mylotinised
orthogneisses and granites of
various degrees. The country rock is
made up of gneiss and amphibolite. In
the Banefo massifs, the orthogneiss is
the least deformed petrographic unit.
It shows a heterogranular granoblastic
texture with a mineral assemblage
formed by quartz, K-feldspars, biotite,
etc., within the orthogneiss, remains of
magmatic fluidality can still be observed
marked by feldspar megacrystal. Field observations reveal a net progression
of the intensity of deformation of
orthogeisses to ultramylotinised granites
having an identical chemical composition
as the orthogneisses...conferenc
A new practical and economical technique for the obtention of high quality thin section photographs with the help of a simple optical microscope
Microscopic study is an indispensable
step in the determination of the petrographic
characteristics of rocks. In
Cameroon just like in most developing
countries, simple polarizing microscopes
of the 20th Century constitute the only
available material for macroscopic studies.
A major difficulty encountered in
the use of these instruments resides in
the realisation of photographs of the different
parts of the thin section that require
illustrations. The technique that
has been used upto now has been inefficient
and unsatisfactory. Faced with
this recurrent situation, we thought of
setting up a new, semi-modern, practical
and very economical technique for
photographing the thin section.conferenc
Neotectonic markers in the Panafrican belt formations of Cameroon: elements of interpretation and their environmental impacts
The North equatorial Panafrican Belt,
whose Cameroonian formations are
dated between 650 and 400 million
years, and which are located in the
North of the Congo Craton, is subdivided
in to three major geodynamic domains:
a north Cameroon domain, a
central Cameroon domain and a south
Cameroon domain. These major domains
are generally, particularly the
central domain, affected by great strikeslip
faults in which the most important
are the central cameroonian shear zone
and the Sanaga fault.
Studies that establish the order of occurrence
of geological events, generally
performed in these domains and particularly
at Banefo area (West Cameroon)
reveal markers of recent tectonics (post
panafrican) that affect the granitogneissic
basement...conferenc