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Research on the high-metamorphic complexes of the Agto area
Author(s) -
E Bondesen
Publication year - 1968
Publication title -
rapport
Language(s) - English
Resource type - Journals
eISSN - 2597-2944
pISSN - 0418-6559
DOI - 10.34194/rapggu.v15.7167
Subject(s) - granulite , metamorphic rock , facies , gneiss , geology , metamorphic facies , field (mathematics) , tectonics , metamorphism , geochemistry , geomorphology , paleontology , mathematics , structural basin , pure mathematics
Mapping in the Agto area was continued in 1967, the second season of new research in this area; five teams were in the field mapping in nine individual areas. The main object of the mapping is to elucidate the relations between the Isortoq granulite facies complex in the south and the amphibolite facies gneisses of the Egedesminde complex in the north (Ramberg, 1949). AIready from the first field season (Bondesen, 1966, p. 20) it was clear that the problem essentially concerned areas with contrasted tectonic development and style besides metamorphic history and degree.

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