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...
Main Authors: | Károly Lázár, Zoltán Máthé, Tibor Németh, Viktória Kovács-Kis, Sándor Stichleutner, Ivett Kovács |
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Format: | Article |
Language: | English |
Published: |
MDPI AG
2024-02-01
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Series: | Minerals |
Subjects: | |
Online Access: | https://www.mdpi.com/2075-163X/14/2/196 |
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