Formation and evolution of Th–REE mineralizing fluids at the Kiruna‐type Choghart iron oxide–apatite deposit, Central Iran: Insights from fluid inclusions and H‐C‐O isotopes
Author:
Affiliation:
1. Nuclear Science and Technology Research Institute Nuclear Fuel Cycle Research School Tehran Iran
2. Department of Geology, Faculty of Earth Science University of Shahid Beheshti Tehran Iran
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4399
Reference63 articles.
1. O and H stable isotope compositions of oceanic crust and upper mantle rocks exposed in the Hess Deep near the Galapagos Triple Junction
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4. Calculation of fractionation factors for carbon and oxygen isotopic exchange in the system calcite-carbon dioxide-water
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1. Determining the genesis of uranium mineralization in Saghand anomaly-2 using geochemistry of rare earth elements in uraninite, Central Iran;Iranian Journal of Crystallography and Mineralogy;2024-07-01
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3. Geology and geochemistry of metasomatite rocks associated with Kiruna iron oxide apatite and the evolution of fluids responsible for metasomatism in Choghart and Chadormalu deposits (Bafq mining district, Central Iran);Arabian Journal of Geosciences;2023-03-14
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