Polyphase deformation at the Harder Fjord Fault Zone (North Greenland)

In North Greenland, the E–W-trending Harder Fjord Fault Zone represents a major lineament which cuts through Cambrian to Silurian deep-water sediments of the Franklinian Basin over a distance of 300 km. On both sides of the fault zone, these successions were affected by two stages of folding (F1, F2...

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Bibliographic Details
Published in:Geological Magazine
Main Authors: PIEPJOHN, K., VON GOSEN, W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2001
Subjects:
Kap
Online Access:http://dx.doi.org/10.1017/s0016756801005660
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756801005660