Constant strain accumulation rate between major earthquakes on the North Anatolian Fault. (2018)
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/10.1038/s41467-018-03739-2
PubMed Identifier: 29643366
Publication URI: http://europepmc.org/abstract/MED/29643366
Type: Journal Article/Review
Volume: 9
Parent Publication: Nature communications
Issue: 1
ISSN: 2041-1723