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" and more evidence of viscous flow. 3. Albite-magnetite-quartz-magma, with abundant smoothwalled vesicles, and evidence of the presence of "
Geologiska föreningens i Stockholm förhandlingar - Page 236
by Geologiska föreningen (Sweden) - 1916
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The Geology and Petrology of the Great Serpentine Belt of New ..., Parts 1-7

William Noël Benson - 1913 - 482 pages
...with a few irregular vesicles, and slight evidence of pneumatolysis. Less brecciation than in No.l, and more evidence of viscous flow. 3. Albite-magnetite-quartz-magma,...smoothwalled vesicles, and evidence of the presence of magmatic water. Still further diminished viscosity, brecciation practically absent, and flow-structures...
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Proceedings of the Linnean Society of New South Wales, Volume 40

Linnean Society of New South Wales - 1916 - 1034 pages
...hydro-pneumatolysis played an important minor rôle. This accords, to a great extent, with the views of 3. Albite-magnetite-quartz-magma, with abundant smoothwalled vesicles, and evidence of the presence of magmatic water. Still further diminished viscosity, brecciation practically absent, ind flow-structures...
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