Figure 5. Field aspects and photomicrographs of the thin sections of the representative basaltic dyke. (a) Field characteristics of the dyke; (b) Hand specimen of the basaltic dykes; (c, d, e and f) Microlitic porphyritic textures showing a large Olivine and pyroxene crystals in mesostase; (e) Olivine with opaque mineral inclusion

From

Petrochemical Characterization of Basaltic Dykes in Nkor Noni Area of Mount Oku, Cameroon Volcanic Line: Constrain on the Source of Magma and the Geotectonic Setting

Tene Djoukam Joëlle Flore, Fontem Kibong Nicoline, Wotchoko Pierre, Chenyi Vohnyui Marie-Louise, Kouankap Nono Gus Djibril

Journal of Geosciences and Geomatics. 2024, 12(3), 62-72 doi:10.12691/jgg-12-3-2