Abstract
The metaluminous Watergums granite, from a bimodal association of A-type granite/rhyolite with basalt in SE Australia, has been experimentally studied so that constraints can be placed on its origin. Petrological, geochemical and experimental data support an origin by direct, high-T partial melting of a melt-depleted I-type source rock in the lower crust.-J.A.Z.
Cite
CITATION STYLE
APA
Clemens, J. D., Holloway, J. R., & White, A. J. R. (1986). Origin of an A-type granite: experimental constraints. American Mineralogist, 71(3–4), 317–324.
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