The depth of pseudotachylyte formation from detailed thermochronology and constraints on coseismic stress drop variability (2012)
Attributed to:
National Environmental Isotope Facility (NEIF)
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1029/2011jb008846
Publication URI: http://dx.doi.org/10.1029/2011jb008846
Type: Journal Article/Review
Parent Publication: Journal of Geophysical Research: Solid Earth
Issue: B6