The role of water-rock interaction on Fe isotope fractionation in continental sandstone aquifers

Published: 23 July 2026| Version 1 | DOI: 10.17632/4nvs2skk3p.1
Contributors:
yuan Liu, Junhong Zhao, Biji Luo

Description

Supplementary Materials: Iron isotope fractionation model in sandstones; Thermodynamic modeling of U-δ56Fe coevolution. Table S1 Whole-rock elements, S contents, and bulk Fe3+/ΣFe ratios of the Zhiluo Formation sandstones in the Nalinggou uranium deposit. Table S2 Whole-rock Fe isotopic compositions of the Zhiluo Formation sandstones in the Nalinggou uranium deposit.

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Geology

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