Evidence of Gondwana early rifting process recorded by Resende-Ilha Grande Dike Swarm, southern Rio de Janeiro, Brazil
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40Ar/39Ar data for Resende-Ilha Grande Tholeiitic Dike Swarm point to early extensional episode ca. 156-144 Ma.

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The event precedes the onset of Paraná LIP and the Gondwana break-up.

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Three high-TiOb>2b> magmatic suites identified using geochemistry and Nd and Sr isotopic data.

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Tb>DMb> ages suggest basement contamination and are similar to mafic rocks interlayered with Neoproterozoic basement.

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The swarm represents the precise onshore projection of Pelotas-Santos rift propagator, in the N–S direction.

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