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