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  1. Lamprophyre dikes as tectonic markers of late orogenic transtension timing and kinematics: a case study from the Central Iberian Zone

    Variscan Central Iberian Zone lamprophyre dikes cut synorogenic to late orogenic peraluminous S-type granitoids marking an important shift in regional tectonic regime from earlier, 350-290 Ma, extension-related crustal melting to […]

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