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    Late Holocene hydrous mafic magmatism at the Paint Pot Crater and Callahan flows, Medicine Lake Volcano, N. California and the influence of H2O in the generation of silicic magmas

    This paper characterizes late Holocene basalts and basaltic andesites at Medicine Lake volcano that contain high pre-eruptive H2O contents inherited from a subduction related hydrous component in the mantle. The...

    R. J. Kinzler, J. M. Donnelly-Nolan… in Contributions to Mineralogy and Petrology (2000)

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    Abrupt shift in δ18O values at Medicine Lake Volcano (California, USA)

     Oxygen-isotope analyses of lavas from Medicine Lake volcano (MLV), in the southern Cascade Range, indicate a significant change in δ18O in Holocene time. In the Pleistocene, basaltic lavas with <52% SiO2 average...

    J. M. Donnelly-Nolan in Bulletin of Volcanology (1998)

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    Evidence of hydrous differentiation and crystal accumulation in the low-MgO, high-Al2O3 Lake Basalt from Medicine Lake volcano, California

    The late Pleistocene Lake Basalt of Medicine Lake volcano, California is comprised of variably porphyritic basalt and basaltic andesite flows and scoria. These eruptives are similar in composition and phenocry...

    T. P. Wagner, J. M. Donnelly-Nolan… in Contributions to Mineralogy and Petrology (1995)

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    Assimilation of granite by basaltic magma at Burnt Lava flow, Medicine Lake volcano, northern California: Decoupling of heat and mass transfer

    At Medicine Lake volcano, California, andesite of the Holocene Burnt Lava flow has been produced by fractional crystallization of parental high alumina basalt (HAB) accompanied by assimilation of granitic crus...

    T. L. Grove, R. J. Kinzler, M. B. Baker… in Contributions to Mineralogy and Petrology (1988)

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    The evolution of young silicic lavas at Medicine Lake Volcano, California: Implications for the origin of compositional gaps in calc-alkaline series lavas

    At Medicine Lake Volcano, California, the compositional gap between andesite (57–62 wt.% SiO2) and rhyolite (73–74 wt.% SiO2) has been generated by fractional crystallization. Assimilation of silicic crust has al...

    T. L. Grove, J. M. Donnelly-Nolan in Contributions to Mineralogy and Petrology (1986)