A new mode of mineral replacement reactions involving the synergy between fluid-induced solid-state diffusion and dissolution-reprecipitation: A case study of the replacement of bornite by copper sulfides

Author:

Adegoke Idowu A.ORCID,Xia FangORCID,Deditius Artur P.,Pearce Mark A.,Roberts Malcolm P.,Brugger Joël

Funder

University of Western Australia

Australian Research Council

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference100 articles.

1. Textural and compositional complexities resulting from coupled dissolution–reprecipitation reactions in geomaterials;Altree-Williams;Earth Sci. Rev.,2015

2. The Carbonatation of Anhydrite: Kinetics and Reaction Pathways;Altree-Williams;ACS Earth Space Chem.,2017

3. Quantitative analysis of silicates and oxide minerals: Comparison of Monte-Carlo, ZAF, and Phi-Rho-Z procedures;Armstrong;Microbeam Anal.,1988

4. Solid solutions in the system Cu-Fe-S, Part I; the Cu-S and CuFe-S joins;Barton;Econ. Geol.,1973

5. On the mechanisms of cation diffusion processes in ternary feldspars;Behrens;Phys. Chem. Miner.,1990

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