Evaluating new fault-controlled hydrothermal dolomitization models: Insights from the Cambrian Dolomite, Western Canadian Sedimentary Basin (2020)
Attributed to:
National Environmental Isotope Facility (NEIF)
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1111/sed.12729
Publication URI: http://dx.doi.org/10.1111/sed.12729
Type: Journal Article/Review
Parent Publication: Sedimentology
Issue: 6