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Pyrothalassite and the evolution of volcanic islands
Published online by Cambridge University Press: 01 May 2009
Summary
It is proposed that the term pyrothalassite should be used to describe the materials that form the outer and upper covering of a volcanic edifice that rises from the sea bed, and it includes the fragmental materials produced by hydroexplosions and surf action in the upper layers of the sea. This material is both porous and enriched in thalassophile elements. These two characteristics give a pyrothalassite layer the ability to exert a profound influence on the magmatic evolution of volcanic islands that contain, or contained, such a layer.
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REFERENCES
Barth, T.F.W. 1968. Petrology of Continental Rocks. Bull. geol. Soc. Finland, 40, 3–9.CrossRefGoogle Scholar
McBirney, A.R. 1963. Factors governing the nature of submarine volcanism. Bull. volcanol. 2, (26), 455–469.CrossRefGoogle Scholar
Melson, W.G., Thompson, G. & van Andel, T.H. 1968. Volcanism and metamorphism in the mid-Atlantic Ridge, 22°N Latitude. J. geophys. Res. 73, (18), 5925–5941.CrossRefGoogle Scholar
Melson, W.G. & van Andel, T.H. 1966. Metamorphism in the mid-Atlantic ridge, 22°N latitude. Marine Geol. 4 (3), 165–186.CrossRefGoogle Scholar
Middlemost, E.A.K. (In press). Volcanic and associated rocks of San Miguel de La Palma. Canary Islands. Proc. geol. Soc. Lond.Google Scholar
Nayudu, Y.R. 1962. A new hypothesis for origin of guyots and seamount terraces. Crust of the Pacific Basin. Geophysical Mon. No. 6, 171–180.Google Scholar
Siever, R. 1968. Establishment of equilibrium between clays and sea water. Earth and Planetary Sci. Letters, 5 (2), 106–110.CrossRefGoogle Scholar
Thorarinsson, S. 1964. Surtsey: A new island in the North Atlantic. Almenna Bokafelagid, Reykjavik.Google Scholar