The structural chronology of the Nigerdlikasik area, Frederikshåbs district

Abstract

In basement areas of good exposure which enable continuous marker horizons to be mapped. it is possibIe to distinguish many events in the structural history. Thus in the Nigerdlikasik areal 45 km due east of Frederikshåb, it has been possibIe to trace at least five phases of deformation and associated migmatization by mapping the many fold closures in amphibolite horizons.