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)

First Author: Saintilan N
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