Figure 8. Structural elements of the second phase of deformation: a) S2 foliation in the amphibole and biotite gneisses of Mazang; b) S2 banding in the banded amphibolite of Boboyo ; c) S2 foliation in the amphibolites of Doumrou; d) S2 foliation in midjivin micaschist; e) S2 foliation in the Morsalé talcschist; f) L2 Mineral and stretching lineation in the Zanoumi amphibolites; g) L2 Mineral and stretching lineation in the biotite gneisses of Zanoumi; h) L2 striae in Guérémé quartzites; i) B2 Boudin of sigmoid quartzo-feldspathic materials in the Zanoumi amphibolites; j) Amphibolite sheared into boudins in Aviation biotite gneiss; k) F2 isopac folds at KéoKéo; i) F2 Anisopac folds at Boboyo; m) F2 Anisopac and dissymmetrical folds at KéoKéo; n) C2 Dextral shear in the banded amphibolites of Boboyo

From

Structural Study of the Precambrian Basement of Kaele (Far North Cameroon): Contribution of Remote Sensing (Application of Landsat 8 OLI/TIRS Images) and Field Data

Bello Bienvenue, Ganwa Alembert Alexandre, Naimou Seguem, Simeni Wambo Armel Nicole, Amadou Diguim Kepnamou, Yingyang Wangbitching Raoul, Haskandi Kalaza Josué

Journal of Geosciences and Geomatics. 2023, 11(1), 1-10 doi:10.12691/jgg-11-1-1