Formation and growth of normal faults at the divergent plate boundary in Iceland

ABSTRACT The divergent plate boundary in Iceland is characterized by 40–80 km long and 5–10 km wide swarms of tension fractures (∼10 2 m long) and normal faults (∼10 3 m long). The upper part of the crust is mainly composed of lava flows, with abundant columnar joints that are mostly perpendicular t...

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Bibliographic Details
Published in:Terra Nova
Main Author: Gudmundsson, Agust
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1992
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1365-3121.1992.tb00582.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3121.1992.tb00582.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3121.1992.tb00582.x