The experimental incorporation of Fe into talc: a study using X-ray diffraction, Fourier transform infrared spectroscopy, and Mössbauer spectroscopy

Author:

Corona Juan Carlos,Jenkins David M.,Dyar M. Darby

Funder

National Science Foundation

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference61 articles.

1. Ahn JH, Buseck PR (1989) Microstructures and tetrahedral strip-width order and disorder in Fe-rich minnesotaites. Am Mineral 74:384–393

2. Angerer T, Hagemann SG, Danyushevsky LV (2012) Geochemical evolution of the banded iron formation-hosted high-grade iron ore system in the Koolyanobbing Greenstone Belt, Western Australia. Econ Geol 107:599–644

3. Bancroft GM, Burns RG (1969) Mössbauer and absorption spectral study of alkali amphiboles. In: Papike JJ (ed) Pyroxenes and amphiboles: crystal chemistry and phase petrology. Mineral Soc Am, Spec Pap 2, pp 137–148

4. Belonoshko A, Saxena SK (1991) A molecular dynamics study of the pressure–volume–temperature properties of supercritical fluids: II. CO2, CH4, CO, O2, and H2. Geochim Cosmochim Acta 55:3191–3208

5. Bose K, Ganguly J (1994) Thermogravimetric study of the dehydration kinetics of talc. Am Mineral 79:692–699

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