In this contribution we present new insights on the evolution of the Dom Feliciano Belt, southernmost Man-tiqueira Province, integrating new whole-rock Sm–Nd i
Quantification of a mineral prospectivity mapping (MPM) heavily relies on geological, geophysical and geochemical analysis, which combines various evidence laye
Chromitite bodies hosted in peridotites typical of suboceanic mantle (s.l. ophiolitic) are found in the northern and central part of the Loma Caribe peridotite,