Iron oxide chemistry supports a multistage hydrothermal genesis of BIF-hosted hematite ore in the Mt. Tom Price and Mt. Whaleback deposits

Author:

Angerer Thomas,Thorne Warren,Hagemann Steffen G.,Tribus Martina,Evans Noreen J.,Savard Dany

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference113 articles.

1. Point defects and cation tracer diffusion in (Ti x Fe 1–x) 3− δ O 4. II. Cation tracer diffusion;Aggarwal;Phys. Chem. Miner.,2002

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

3. Angerer, T., Hagemann, S.G., Boyce, A.J., Reichardt, H., 2013a. Mt. Whaleback: chemical constraints on the genesis of the largest hematite ore body in the Hamersley Province, Australia, Mineral deposit research for a high-tech world. Proceedings of the 12th Biennial SGA Meeting, 12–15 August 2013, Uppsala, Sweden, ISBN 978-91-7403-207-9, pp. 708-711.

4. Angerer, T., Hagemann, S.G., Danyushevsky, L., 2011. Monitoring geochemical processes in BIF-hosted iron ore, Yilgarn craton, by using a combination of whole rock and in situ laser ablation ICP-MS analyses, Conference Proceedings, SGA 2011, Antofagasta, Chile. Ediciones Universidad Catolica del Norte, Antofagasta, Chile, pp. 190-192.

5. High-grade iron ore at Windarling, Yilgarn Craton: a product of syn-orogenic deformation, hypogene hydrothermal alteration and supergene modification in an Archean BIF-basalt lithostratigraphy;Angerer;Miner. Deposita,2013

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