Deep magnetotelluric signatures of the early Neoproterozoic Cariris Velhos tectonic event within the Transversal sub-province of the Borborema Province, NE Brazil
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文摘

New lithospheric model for central Borborema Province from magnetotelluric inversion.

North-dipping crustal conductors interpreted as remnants of subduction zone.

Early Neoproterozoic rocks with oceanic affinity constrain age of subduction event.

Accretionary model supported for geodynamic evolution of the Borborema Province.

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