Publication Date:
1948-08-01
Description:
The formation of a fold mountain chain is, essentially, a thermal phenomenon, as may be deduced from the internal locus of the forces involved, the frequent association of magrriatic activity with erogenic movements, and the widespread thermal and regional metamorphism of the sediments within the deeper parts of the mountain belt.
Print ISSN:
0016-7568
Electronic ISSN:
1469-5081
Topics:
Geosciences
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