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Implications of the low-angle normal (evolving) crustal shear-zone model for metamorphic core complexes of Cordilleran type, and the origin of the ‘accretionary wedge’ of the Hellenic arc : G. S. Lister, Bureau of Mineral Resources, P.O. Box 378, Canberra, A.C.T., Australia, 2601


Book ID
118404126
Publisher
Elsevier Science
Year
1985
Tongue
English
Weight
306 KB
Volume
7
Category
Article
ISSN
0191-8141

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