Relating differential crustal architecture to passive margin evolution: A case study from the Colatina Fracture Zone (SE Brazil) using apatite fission‐track thermochronology
Deniro Felipe Gonçalves Costa,
Ana Fonseca,
Johan de Grave
et al.
Abstract:The Colatina Fracture Zone (CFZ) defines a distinct NNW–SSE‐oriented linear zone of fractures and brittle faults that represents an inherited weak zone in the current crustal structure of the (Pre)Cambrian Araçuaí Orogen. In the Early Cretaceous, the CFZ was reactivated during rifting of West Gondwana and subsequent opening of the South Atlantic Ocean, as evidenced by the emplacement of dykes along its structural network and the development of major depocentres of the Campos Basin in the offshore segments of t… Show more
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