Abundant high-K calc-alkaline HKCA magmatism appears to be post-collisional
and often shifts to shoshonitic or alkaline–peralkaline compositions in the final
Contrasting origin of post-collisional high-K calc-alkaline and shoshonitic versus alkaline and ... PDF
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Abundant high-K calc-alkaline HKCA magmatism appears to be post-collisional
and often shifts to shoshonitic or alkaline–peralkaline compositions in the final
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