Constraining the maximum depth of brittle deformation at slow- and ultraslow-spreading ridges using microseismicity (2019)
Attributed to:
Crustal accretion and transform margin evolution at ultraslow spreading rates
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1130/g46577.1
Publication URI: http://dx.doi.org/10.1130/g46577.1
Type: Journal Article/Review
Parent Publication: Geology
Issue: 11