Reactivation of fault systems by compartmentalized hydrothermal fluids in the Southern Andes revealed by magnetotelluric and seismic data. (2020)
Attributed to:
Time-dependent deformation: bridging the strain rate gap in brittle rocks.
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Type: Journal Article/Review
Volume: 39
Parent Publication: Tectonics