Dike intrusions during rifting episodes obey scaling relationships similar to earthquakes

As continental rifts evolve towards mid-ocean ridges, strain is accommodated by repeated episodes of faulting and magmatism. Discrete rifting episodes have been observed along two subaerial divergent plate boundaries, the Krafla segment of the Northern Volcanic Rift Zone in Iceland and the Manda-Har...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: L. , Passarelli, E. , Rivalta, A. , Shuler
Other Authors: L., Passarelli, E., Rivalta, A., Shuler
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/11585/775991
https://doi.org/10.1038/srep03886
https://www.nature.com/articles/srep03886