Metamorphism, Metasomatism and Conditions of Formation of Industrial Minerals of the Sillimanite Group of the Fennoscandian Shield

<p id="p1">The group of sillimanite minerals includes kyanite, sillimanite and andalusite, modifications. It is shown that high-alumina complexes are widespread throughout the Fennoscandian Shield, but the sources (protoliths) are sedimentary-volcanogenic formations of the preceding stages. Three me...

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Autor principal: Shchiptsov, Vladimir
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Lenguaje:inglés
Publicado: IntechOpen 2024
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Acceso en línea:https://www.intechopen.com/chapters/1168876
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