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Publikováno v:
Hyperfine Interactions. :61-71
Serpentine “polymorph” minerals (chrysotile, lizardite, and antigorite) are hydrous Mg–Fe silicates that commonly form serpentine rock (serpentinite) by hydration of olivine-pyroxene peridotites from the mantle of the Earth. During the complex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fedbba4f97270e14fb3147f1f942545f
https://doi.org/10.1023/b:hype.0000003765.32151.3b
https://doi.org/10.1023/b:hype.0000003765.32151.3b
