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The Deep Proterozoic Crust in the North Atlantic Provinces (Paperback, 1985 ed.)
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The Deep Proterozoic Crust in the North Atlantic Provinces (Paperback, 1985 ed.)
Series: NATO Science Series C, 158
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The Proterozoic terrains of South Scandinavia and the Grenville
Province in North-America have many common features: Regional high
grade metamorphism (Granulite-facies), anorthosites, etc. They are
separated by the Caledonian orogeny and, above all, by the Atlantic
Ocean. During the time of the great continental drift controversy,
few people were ready to admit that both sides on the Atlantic were
once an unique province. Now everybody agrees on the Post-paleozoic
age of the Atlantic and, consequently, on the intrinsic homogeneity
of the much older. rocks which occur around it. But a detailed
comparison is not easy. The Grenville Province is much larger than
South Scandinavia, both regions have been investigated by a great
number of different schools, using various methods, approaches and
concepts. After several attempts, and long discussion, it was felt
by a small group of individuals, that literature study would not be
enough and that nothing could re place the direct contact, in the
field, of specialists who had a first hand knowledge of all
involved regions. The formula of a NATO Advanced Study Institute,
which gives a unique opportunity to meet and mix people of various
origin and levels, came almost by itself. Much work was needed,
much help has been obtained, as detailed in the
"Acknowledgements.""
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