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“Endogenous growth in channelized komatiite lava flows; evidence from spinifex-textured sills at Pyke Hill and Serpentine Mountain, western Abitibi greenstone belt, northeastern Ontario, Canada”, Bulletin of Volcanology, vol. 71, pp. 881-901, 2009.
, GeoRef, Copyright 2018, American Geological Institute.2014-011844northeastern OntarioPyke HillSerpentine Mountain
“Endogenous growth in channelized komatiite lava flows: evidence from spinifex-textured sills at Pyke Hill and Serpentine Mountain, Western Abitibi Greenstone Belt, Northeastern Ontario, Canada”, Bulletin of VolcanologyBulletin of Volcanology, vol. 71, pp. 881-901, 2009.
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