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Reply to comments by J. H. Bédard and R. S. J. Sparks

Published online by Cambridge University Press:  03 November 2011

J. A. Volker  and
B. G. J. Upton
J. A. Volker
Affiliation:
Saint-Maurice-de-Tanernale, 17500, Jonzac, France.
B. G. J. Upton
Affiliation:
Department of Geology and Geophysics, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, U.K.
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Extract

Bédard and Sparks' (BS) comments are very much appreciated as they giveus the opportunity to emphasise certain aspects of our observations which, in turn, mayclarify the discussion on the petrogenesis of the Rhum ultrabasic rocks. BS raised two questions which we answer below.

Type
Reply
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 82 , Issue 4 , 1991 , pp. 391
Copyright
Copyright © Royal Society of Edinburgh 1991

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References

Bédard, J. H., Sparks, R. S. J., Renner, R., Cheadle, M. J. & Hallworth, M. A. 1988. Peridotite sills and metasomatic gabbros in the Eastern Layered Series of the Rhum complex. J GEOL SOC LONDON 145, 207–24.CrossRefGoogle Scholar
Brown, G. M. 1956. The layered ultrabasic rocks of Rhum, Inner Hebrides. PHILOS TRANS ROY SOC LONDON B240, 1–53.Google Scholar
Huppert, H. E. & Sparks, R. S. J. 1980. The fluid dynamics of a basaltic magma chamber replenished by influx of hot, dense, ultrabasic magma. CONTRIB MINERAL PETROL 75, 275–89.Google Scholar
Young, I. M. & Donaldson, C. H. 1985. Formation of granular textured layers and laminae within the Rhum crystal pile. GEOL MAG 122, 519–28.CrossRefGoogle Scholar