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Peridotite-Gabbro Complexes as Keys to Petrology of Mid-Oceanic Ridges: Discussion

D. H. Green
D. H. Green
Mintralogisk Museum, Osle, Norway
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January 01, 1976


(Thayer 1969) has drawn attention to characteristics of several ultramafic occurrences with the theme that studies of such complexes exposed in orogenic belt may lead to understanding of processes currently operating at the mid- oceanic ridges. The author supports this approach, but considers that Thayer is incorrect in attempting to reduce these particular occurrences to a common denominator of olivine- rich ultramafic and comagmatic gabbroic rocks, and in neglecting important differences in the chemical composition, mineralogy and emplacement mechanism of various ultramafics. There is disagreqpent on geological interpretations which have led the author to postulate, for sope ultramafic complexes,-a history with high pressure, high temperature crystallization, and Bigh temperature emplacement at shallow levels as hot crystalline ultramafic diapirs.

This discussion will focus on aspects of such an intrusion (Lizard, Cornwall) disputed by Thayer (1967, 1969), -and develop from this a more detailed model of inter-relationships between ultramafic and basaltic rocks at the mid-oceanic ridges.

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GSA Microform Publications

Mid-Atlantic Ridge

Peter A. Rona
Peter A. Rona
National Oceanic and Atmospheric Administration Atlantic Oceanographic and Meteorological Laboratories 15 Rickenbacker Causeway Miami, Florida 33149
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Geological Society of America
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Publication date:
January 01, 1976




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