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

  • J. A. Volker (a1) and B. G. J. Upton (a2)
  • In response to commentaries on:

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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.

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References

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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.
Brown, G. M. 1956. The layered ultrabasic rocks of Rhum, Inner Hebrides. PHILOS TRANS ROY SOC LONDON B240, 153.
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.
Young, I. M. & Donaldson, C. H. 1985. Formation of granular textured layers and laminae within the Rhum crystal pile. GEOL MAG 122, 519–28.

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

  • J. A. Volker (a1) and B. G. J. Upton (a2)
  • In response to commentaries on:

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