The role of magma mixing and mafic recharge in the evolution of a back-arc quaternary caldera: The case of Payún Matrú, Western Argentina
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文摘

Textural and mineralogical disequilibrium in lavas are common in Payún Matrú.

Magma mixing and mingling processes have been recurrent in Payún Matrú volcano.

Trigger mechanism for the caldera-forming eruption was probably a mafic recharge.

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