Crystals structures of carbonate phases with Mg in Triassic rocks, mineral formation and transitions

Abstract Detailed data on carbonate minerals different in magnesium content including their crystal structures were presented in this article. The samples were collected from the formations of the Lower Muschelkalk and the Upper Muschelkalk. X-ray diffraction and electron microprobe analysis were us...

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Main Author: Katarzyna J. Stanienda-Pilecki
Format: Article
Language:English
Published: Nature Portfolio 2023-10-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-023-46013-2
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author Katarzyna J. Stanienda-Pilecki
author_facet Katarzyna J. Stanienda-Pilecki
author_sort Katarzyna J. Stanienda-Pilecki
collection DOAJ
description Abstract Detailed data on carbonate minerals different in magnesium content including their crystal structures were presented in this article. The samples were collected from the formations of the Lower Muschelkalk and the Upper Muschelkalk. X-ray diffraction and electron microprobe analysis were used for carbonate phases determination. The following minerals with different Mg content were identified: low-Mg calcite, high-Mg calcite, proto-dolomite, ordered dolomite and de-huntite. The content of Mg in high-Mg calcite is higher than in low-Mg calcite but lower than that of proto-dolomite. Proto-dolomite is characterized by lower content of Mg than typical for stoichiometric value for dolomite—ordered dolomite. Due to the reduced Mg content in identified huntite, this carbonate phase was named as de-huntite. The research results are significant because they are a source of new data on carbonate phases with different Mg content which build studied Triassic rocks and crystal structures of these minerals.
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spelling doaj.art-d7ef2a0ec660477ca83b2f72acf5303c2023-11-05T12:14:16ZengNature PortfolioScientific Reports2045-23222023-10-0113111210.1038/s41598-023-46013-2Crystals structures of carbonate phases with Mg in Triassic rocks, mineral formation and transitionsKatarzyna J. Stanienda-Pilecki0Department of Applied Geology, Silesian University of TechnologyAbstract Detailed data on carbonate minerals different in magnesium content including their crystal structures were presented in this article. The samples were collected from the formations of the Lower Muschelkalk and the Upper Muschelkalk. X-ray diffraction and electron microprobe analysis were used for carbonate phases determination. The following minerals with different Mg content were identified: low-Mg calcite, high-Mg calcite, proto-dolomite, ordered dolomite and de-huntite. The content of Mg in high-Mg calcite is higher than in low-Mg calcite but lower than that of proto-dolomite. Proto-dolomite is characterized by lower content of Mg than typical for stoichiometric value for dolomite—ordered dolomite. Due to the reduced Mg content in identified huntite, this carbonate phase was named as de-huntite. The research results are significant because they are a source of new data on carbonate phases with different Mg content which build studied Triassic rocks and crystal structures of these minerals.https://doi.org/10.1038/s41598-023-46013-2
spellingShingle Katarzyna J. Stanienda-Pilecki
Crystals structures of carbonate phases with Mg in Triassic rocks, mineral formation and transitions
Scientific Reports
title Crystals structures of carbonate phases with Mg in Triassic rocks, mineral formation and transitions
title_full Crystals structures of carbonate phases with Mg in Triassic rocks, mineral formation and transitions
title_fullStr Crystals structures of carbonate phases with Mg in Triassic rocks, mineral formation and transitions
title_full_unstemmed Crystals structures of carbonate phases with Mg in Triassic rocks, mineral formation and transitions
title_short Crystals structures of carbonate phases with Mg in Triassic rocks, mineral formation and transitions
title_sort crystals structures of carbonate phases with mg in triassic rocks mineral formation and transitions
url https://doi.org/10.1038/s41598-023-46013-2
work_keys_str_mv AT katarzynajstaniendapilecki crystalsstructuresofcarbonatephaseswithmgintriassicrocksmineralformationandtransitions