Motion in the north Iceland volcanic rift zone accommodated by bookshelf faulting

Along mid-ocean ridges the extending crust is segmented1 on length scales of 10–1,000 km. Where rift segments are offset from one another, motion between segments is accommodated by transform faults that are oriented orthogonally to the main rift axis. Where segments overlap, non-transform offsets w...

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Bibliographic Details
Published in:Nature Geoscience
Main Authors: Green, Robert G., White, Robert S., Greenfield, Tim
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2013
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/2972/
http://eprints.esc.cam.ac.uk/2972/1/Green_ngeo_Preprint.pdf
http://eprints.esc.cam.ac.uk/2972/7/ngeo2012-f1.jpg
http://eprints.esc.cam.ac.uk/2972/12/ngeo2012-s1.pdf
http://eprints.esc.cam.ac.uk/2972/13/ngeo2012-s2.xlsx
https://doi.org/10.1038/ngeo2012