Iron K-edge X-ray absorption near-edge structure spectroscopy of aerodynamically levitated silicate melts and glasses-Reference-Cited by-同舟云学术

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Iron K-edge X-ray absorption near-edge structure spectroscopy of aerodynamically levitated silicate melts and glasses

Published:2017-03 Issue: Volume:453 Page:169-185
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Alderman O.L.G.,Wilding M.C.,Tamalonis A.,Sendelbach S.,Heald S.M.,Benmore C.J.,Johnson C.E.,Johnson J.A.,Hah H.-Y.,Weber J.K.R.

Funder

U.S. Department of Energy

Center for Laser Applications

University of Tennessee Space institute

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference106 articles.

1. Structure of molten titanium dioxide;Alderman;Phys. Rev. B,2014

2. Continuous structural transition in glass-forming molten titanate BaTi2O5;Alderman;J. Phys. Chem. C,2016

3. Temperature-driven structural transitions in molten sodium borates Na2O-B2O3: X-ray diffraction, thermodynamic modelling and implications for topological constraint theory;Alderman;J. Phys. Chem. C,2016

4. Local Structural Variation With Oxygen Fugacity in Fe2SiO4+x Fayalitic Iron Silicate Melts;Alderman;Geochim. Cosmochim. Ac.,2017

5. Thermochemical Data of Pure Substances;Barin,1993

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