Weak ductile shear zone beneath a major strike-slip fault: Inferences from earthquake cycle model constrained by geodetic observations of the western North Anatolian Fault Zone (2014)
Attributed to:
Deep crustal structure of the North Anatolian Fault Zone and the earthquake cycle
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1002/2013jb010347
Publication URI: http://dx.doi.org/10.1002/2013jb010347
Type: Journal Article/Review
Parent Publication: Journal of Geophysical Research: Solid Earth
Issue: 4