Synchronous egress and ingress fluid flow related to compressional reactivation of basement faults: the Phoenix and Gryphon uranium deposits, southeastern Athabasca Basin, Saskatchewan, Canada
Crossref DOI link: https://doi.org/10.1007/s00126-017-0737-5
Published Online: 2017-05-06
Published Print: 2018-02
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Li, Zenghua
Chi, Guoxiang
Bethune, Kathryn M.
Eldursi, Khalifa
Thomas, David
Quirt, David
Ledru, Patrick
Funding for this research was provided by:
Natural resources of Canada (TGI)
Cameco Corp.
AREVA Resources Canada Inc.
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