Structure of the Ravns Storø amphibolite belt in the Fiskenæsset region

L.S Andersen; C Friend

doi:10.34194/rapggu.v51.7324

Structure of the Ravns Storø amphibolite belt in the Fiskenæsset region

Authors

L.S Andersen
C Friend

DOI:

https://doi.org/10.34194/rapggu.v51.7324

Abstract

The Ravns Storø belt of metamorphosed plutonic and volcanic rocks is situated on the northern side of Frederikshåbs Isblink (see map plate 1). Its strike varies from NNE to ENE, and it dips steeply towards the SE. The exposed part of the belt is 25 km long with a maximum thickness of 4 km.

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Published

1973-01-01

How to Cite

Andersen, L., & Friend, C. (1973). Structure of the Ravns Storø amphibolite belt in the Fiskenæsset region. Rapport Grønlands Geologiske Undersøgelse, 51, 37–40. https://doi.org/10.34194/rapggu.v51.7324

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Issue

Vol. 51 (1973): Progress report on the geology of the Fiskenæsset region, South-West Greenland

Section

Article

License

This article is distributed under a CC-BY 4.0 licence, permitting free redistribution and reproduction for any purpose, even commercial, provided proper citation of the original work. Author(s) retain copyright over the article contents.