Geology Reference
In-Depth Information
Fig. 9 a and b The diamictite
from the Bou-Azzer inlier ( a ) and
from the Siroua inlier ( b ). c and
d Features of the Anti-Atlas
major fault. c Shear zone with
network of sigmoidal slip
surfaces; the shear zone transects
shales (which are splintered) and
diamicitite. d Closeup of
conglomerate within the shear
zone with fracture surfaces and
fragmented pebbles
Fig. 10 Overview of contact
between Palaeoproterozoic
basement and Ouarzazate Group
and the Tata Group. Inset shows
contact marked by micro-
conglomerates and thin layers of
rhyolitic tuff
Fig. 11 Jbel Kissane showing
well layered sequence of
sedimentary rocks of Ordovician
age
Search WWH ::




Custom Search