Pan-African tectono-thermal evolution of metamorphic complexes in Sinai: Transition from continental-arc collision to back-arc rifting in northern Gondwana (Submitted)
Abstract Amalgamation of supercontinents coincides with dramatic changes of the thermal structural of Earth’s lithosphere that can be observed as different mineral parageneses. Pan-African metamorphic complexes of the Sinai Peninsula (i.e. Feiran-Solaf, Taba and Kid) are studied here to reveal the complex tectono-thermal history that characterizes the amalgamation of the…
