High-Temperature Evolution of Point Defect Equilibria in Hydrous Forsterite Synthesized at 1100 °C a...
High-Temperature Evolution of Point Defect Equilibria in Hydrous Forsterite Synthesized at 1100 °C and up to 4 GPa
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Basel: MDPI AG
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English
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Basel: MDPI AG
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Water distribution in the deep Earth represents one of the most important topics in the field of geodynamics due to its large impact on the physical and chemical properties of the Earth’s mantle, such as electrical conductivity, seismic anisotropy, diffusion, and rheology. In this study, we synthesized hydrous forsterite at 1100 °C and up to 4 GPa...
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High-Temperature Evolution of Point Defect Equilibria in Hydrous Forsterite Synthesized at 1100 °C and up to 4 GPa
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TN_cdi_proquest_journals_2312012208
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2312012208
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ISSN
2075-163X
E-ISSN
2075-163X
DOI
10.3390/min9100574
