Aea. Elmouraouah et al., THE GRANITIC BODIES OF THE HIGH MOULOUYA - GRANITIC LACCOLITHS IN THEEASTERN MESETA OF MOROCCO, Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 317(11), 1993, pp. 1469-1476
The High-Moulouya granites from Aouli and Bou-Mia contain magmatic str
uctures, generated during emplacement in the crust, which provide evid
ence for laccolithic injection. The first magmas, injected along norma
l faults, were gabbroic in composition and cause a partial melting of
pelitic country-rocks. Evidence for magmatic mixing is provided by var
ious enclaves in the granitoids. Granitoid emplacement in the oriental
Meseta occurred in structural transtensional environment, compatible
with the structures of the occidental Meseta.