By Richard T. Haworth (auth.), Paul E. Schenk, R. T. Haworth, J. D. Keppie, W. E. Trzcienski, P. F. Williams, G. Kelling (eds.)
The classical Appalachian, Caledonian, Hercynian, and Mauritanide orogens at the moment are in basic terms segments of a once-continuous Paleozoic mountain belt which has been fragmented in the course of Mesozoic-Cenozoic formation of the North Atlantic Ocean. those segments are significant components of the nations surrounding the North Atlantic - so much of that are participants of NATO. the purpose of this NATO convention used to be to guage those fragments when it comes to their pre-Mesozoic positions, and to aim a synthesis in their geologic evolution on a global and orogen-wide scale. Geologists who've studied those scattered remnants were separated via either geography and self-discipline. Orogen-wide syntheses have beeen tried some time past by means of people who are experts not just in self-discipline but additionally in geography; for that reason, those makes an attempt haven't been passable to each person. This convention introduced jointly the major experts in numerous disciplines from each one nation. They tried to coach different experts, not just of their personal fields, yet in different disciplines, approximately nearby adaptations and specific difficulties. The ensuing foreign cross-fertilization, either inside and among speciaLties, enriched person staff and helped to supply a multi-disciplinary assessment of the orogen.
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177-208. COMPILATION OF CANADIAN MAGNETIC ANOMALY MAPS: A STATUS REPORT Peter J. Hood Geological Survey of Canada, Ottawa 601 Booth Street, Ottawa, Canada KIA OE8 ABSTRACT The first 1:5 M national magnetic anomaly map (MAM) was published by the Geological Survey of Canada in 1967 and subsequent versions were published in 1972 and 1977. The coloured MAM of Canada demonstrated that features of large areal extent such as geological provinces were readily delineated and proved the usefulness of producing such regional compilations.