Synsedimentary to Diagenetic Cu±Co Mineralization in Mesoproterozoic Pyritic Shale Driven by Magmatic-Hydrothermal Activity on the Edge of the Great Falls Tectonic Zone-Black Butte, Helena Embayment, Belt-Purcell Basin, USA: Evidence from Sulfide Re-Os Isotope Geochemistry (2021)
Attributed to:
National Environmental Isotope Facility (NEIF)
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.2113/2021/7866186
Publication URI: http://dx.doi.org/10.2113/2021/7866186
Type: Journal Article/Review
Parent Publication: Lithosphere
Issue: 1