Graphite does not function as a direct reducing agent for unconformity-related uranium mineralization – Evidence from the graphitic metapelite-hosted Gryphon uranium deposit, northern Saskatchewan, Canada-Reference-Cited by-同舟云学术

Graphite does not function as a direct reducing agent for unconformity-related uranium mineralization – Evidence from the graphitic metapelite-hosted Gryphon uranium deposit, northern Saskatchewan, Canada

Published:2023-09 Issue: Volume:15 Page:100028
ISSN:2666-2612
Container-title:Ore and Energy Resource Geology
language:en
Short-container-title:Ore and Energy Resource Geology

Author:

Young Nahanni,Chi Guoxiang^ORCID,Liu Yongxing,Song Hao

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference43 articles.

1. Unconformity-associated uranium deposits of the Athabasca Basin, Saskatchewan and Alberta;Jefferson;GSC Bull.,2007

2. 8: Basins and Uranium Deposits;Kyser,2015

3. Fluid sources in basement-hosted unconformity–uranium ore systems: tourmaline chemistry and boron isotopes from the Patterson Lake corridor deposits, Canada;Potter;Geochem. Explor. Environ. Anal.,2022

4. Fluid evolution along the Patterson Lake corridor in the southwestern Athabasca Basin: constraints from fluid inclusions and implications for unconformity-related uranium mineralization;Rabiei;Geochem. Explor. Environ. Anal.,2021

5. Spatial variations in fluid composition along structures hosting unconformity-related uranium deposits in the Athabasca Basin, Canada: implications for ore-controlling factors;Rabiei;Miner. Deposita,2023

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1. Coupling of thermal convection and basin-basement fluid mixing is critical for the formation of unconformity-related uranium deposits: Insights from reactive transport modeling;Chemical Geology;2023-12