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A contribution to the geochemistry of “Egyptian Alabaster”

Beitrag zur geochemie des „Ägyptischen Alabasters”

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Summary

Egyptian Alabaster” (marble) exhibits a variety of structures the most common of which are: botryoidal structure, banding, cockade structure, vugs and cavities. Banding which is a characteristic feature consists of alternating translucent and white bands of different sizes. The mineralogical composition of the translucent bands has been determined as magnesian calcite and that of the milky-white bands as normal calcite. Differences in the Ca/Mg and Sr/Ca ratios between both types of bands have been noticed and are attributed to differences in the solubilities of Ca−, Mg−, and Sr-carbonates. The origin of the marble is discussed and is considered to be the product of recrystallization of limestone.

Zusammenfassung

„Agyptischer Alabaster” (Marmor) zeigt eine Reihe von Strukturen, von denen am häufigsten sind: traubige Struktur, Bänderung, Kokarden-Struktur, drusige und löchrige Struktur. Die charakteristische Bänderung besteht aus abwechselnd durchscheinenden und weißen Bändern wechselnder Stärke. Die mineralogische Zusammensetzung der durchscheinenden Bänder wurde als Mg-haltiger Calcit und die der milchig-weißen Bänder als gewöhnlicher Calcit bestimmt. Unterschiede im Ca/Mg- und Sr/Ca-Verhältnis zwischen den beiden Typen der Bänder wurden beobachtet; sie werden Löslichkeitsunterschieden der Ca−, Mg− und Sr-Karbonate zugeordnet. Die Genese des Marmors wird diskutiert; er wird als Rekristallisationsprodukt von Kalkstein angesehen.

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El-Hinnawi, E.E., Loukina, S.M. A contribution to the geochemistry of “Egyptian Alabaster”. TMPM Tschermaks Petr. Mitt. 17, 215–221 (1972). https://doi.org/10.1007/BF01085995

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  • DOI: https://doi.org/10.1007/BF01085995

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