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The Topsails igneous terrane, Western Newfoundland: evidence for magma mixing

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Abstract

The Topsails igneous terrane of Western Newfoundland contains a diverse suite of igneous rocks, but consists mainly of Silurian alkaline to peralkaline granites and rhyolites. The terrane exhibits evidence for the coexistence of mafic and salic magmas in the form of composite dykes and flows, sinuous, boudined mafic dykes cutting granites and net vein complexes. Field data and major and trace element chemical data suggest that these magmas mixed to produce limited volumes of more or less homogeneous hydrids.

Magma mixing, a process which has received recent prominence in petrogenetic models for calc-alkaline volcanic suites, has elicited less attention than restite separation and fractional crystallization as a cause of chemical dispersion in granites. Evidence from the Topsails igneous terrane suggests the possible importance of magma mixing to granite petrogenesis and a major role for transcurrent faulting in the origin and evolution of peralkaline magmas.

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Authors and Affiliations

  1. Geological Survey of Canada, 601 Booth Street, K1A OE8, Ottawa, Canada

    Joseph B. Whalen & Kenneth L. Currie

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  1. Joseph B. Whalen
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  2. Kenneth L. Currie
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Whalen, J.B., Currie, K.L. The Topsails igneous terrane, Western Newfoundland: evidence for magma mixing. Contr. Mineral. and Petrol. 87, 319–327 (1984). https://doi.org/10.1007/BF00381288

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  • DOI: https://doi.org/10.1007/BF00381288

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