Felsic melts differentiating to more mafic compositions through crystal uptake: a case of felsic parental arc magmas for mafic lava flows at Taranaki volcano, New Zealand | Zendy

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Felsic melts differentiating to more mafic compositions through crystal uptake: a case of felsic parental arc magmas for mafic lava flows at Taranaki volcano, New Zealand

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