Figure 10. Main structures observed in the field: (a) fault plane filled by a microgranite; (b) normal fault plane filled by a quartzo-feldspathic vein in the stream bed of the Dorguene; (c) C₃ shear affecting an amphibolite vein in the amphibole granite; (d) W-E oriented pegmatite vein in the Gomtalla syenite; (e) C₂/S₂ composite shear, the symmetrical boudin of the stretched-tailed quartzo-feldspathic level is noted; (f) parallel fracture planes followed by the Gambaka stream.

From

Morphotectonic Analysis of Mboula Area in Relation with Central Cameroon Shear Zone (CCSZ) and Lithology Using Remote Sensing and Field Data

Awé Wangméné Salomon, Tchameni Rigobert, Daouda Dawaï, Amadou Diguim Kepnamou, Danra Moh Guela Guy Basile, Haskandi Kalaza Josué, Bayanbé Gaoussou, Sini André

• Previous
• Figure 10 of 15  (Figures index)
• Next