Iron-Bearing Minerals in the Boda Claystone Formation: Correspondences with Stages of Evolution Revealed by Mössbauer Spectroscopy

Iron-Bearing Minerals in the Boda Claystone Formation: Correspondences with Stages of Evolution Revealed by Mössbauer Spectroscopy

The Boda Claystone Formation (BCF) is an extended sedimentary sequence formed in a shallow-water salt lake under semi-arid to arid climatic conditions during the middle Permian period. The rock was formed predominantly from denuded and altered products of three primary felsic sources, the Mórágy Met...

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Bibliographic Details
Main Authors: Károly Lázár, Zoltán Máthé, Tibor Németh, Viktória Kovács-Kis, Sándor Stichleutner, Ivett Kovács
Format: Article
Language:English
Published: MDPI AG 2024-02-01
Series:Minerals
Subjects:
Boda Claystone Formation
Fe<sup>2+</sup> and Fe<sup>3+</sup> in sheet silicates
clays
Mössbauer spectroscopy
illite
chlorite
Online Access:https://www.mdpi.com/2075-163X/14/2/196

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https://www.mdpi.com/2075-163X/14/2/196

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