The Significance of Heat Transport by Shallow Fluid Flow at an Active Plate Boundary: The Southern Alps, New Zealand (2018)
Attributed to:
Geothermal systems related to rapid uplift on the Alpine Fault, New Zealand
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1029/2018gl078692
Publication URI: http://dx.doi.org/10.1029/2018gl078692
Type: Journal Article/Review
Parent Publication: Geophysical Research Letters
Issue: 19