Research on the high-metamorphic complexes of the Agto area

Abstract

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.