Tectonic Features of the Hecla Hook Formation to the South of St. Jonsfjord, Vestspitsbergen
Abstract A structural study of rocks of the Hecla Hook formation in the area of Forlandsundet of Vestspitsbergen reveals the presence of two B –axes. The earlier ( B 1 ) trends roughly east–west and affects only the Hecla Hook formation; the later axis ( B 2 ) trends roughly north–south, and affects...
Published in: | Geological Magazine |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1953
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0016756800065468 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800065468 |
Summary: | Abstract A structural study of rocks of the Hecla Hook formation in the area of Forlandsundet of Vestspitsbergen reveals the presence of two B –axes. The earlier ( B 1 ) trends roughly east–west and affects only the Hecla Hook formation; the later axis ( B 2 ) trends roughly north–south, and affects also rocks of Carboniferous age. It is suggested that B 1 is the main “Caledonian” axis in this area, and that B 2 and the roughly north–south “grain” of the rocks concerned are Lower Tertiary phenomena. |
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