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Long-lived, stationary magmatism and pulsed porphyry systems during Tethyan subduction to post-collision evolution in the southernmost Lesser Caucasus, Armenia and Nakhitchevan

Earth ScienceVolcanologyTethyan SubductionEngineeringIgneous PetrogenesisTectonic EvolutionSouthernmost Lesser CaucasusGeologyIgneous ProcessStationary MagmatismOrogenyPetrologyTectonics