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Multi-stage fault formation and REE distribution in the surrounding Devonian dolomites in the south-eastern part of the Holy Cross Mountains (Poland)

Nieć Marek, Pawlikowski Maciej, Sermet Edyta

Geology, Geophysics and Environment

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2024

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Vol. 50, no. 1

77--92

EN

Metallogenic studies carried out in the Holy Cross Mountains indicate a relationship between mineralization and fault tectonics in Devonian formations. The impact of fault formation on the geochemistry of host rocks has not yet been studied. Mineralogical and geochemical studies of fault core gouges and damage zones in the fault walls of Devonian dolomites in the Budy and Jurkowice quarries were carried out. In the clay-carbonate filling of the fault fissure, the presence of two generations of Fe sulfides, the increased content of Zr, Nb, U and Th in relation to the surrounding rocks was noted. In the fault walls of the dolomites, iron sulfide and hematite mineralization were found. Research on the REE content indicates that it is lower in the fault walls than in those located far from it, while it is clearly higher in the fault gouge, especially in terms of the content of “heavy” elements (HREE). This indicates both the supply of some components to the fault zone from external sources and their displacement from the surrounding rocks. It was also found that the fault was renewed before and after the Neogene at least twice (Badenian).

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Wybrane zagadnienia biomineralogii

Pawlikowski Maciej

Przegląd Geologiczny

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2022

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Vol. 70, nr 11

834--839

EN

Biomineralogy is the science between mineralogy, biology, medicine and biochemistry. It is focused on problems concerning mineralization of tissue and organs of human, animals and flora. It concerns interaction between mineral and biological tissue, as well as between biochemical components of living organism. These processes are important for good functioning of organs and human life.

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Prefabrykowane panele z aktywną izolacją termiczną

Pawlikowski Maciej, Fedorczak-Cisak Małgorzata, Romańska-Zapała Anna, Wiśniowska Aleksandra

Materiały Budowlane

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2021

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nr 11

25--27

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Dolomite-illitic rocks (dolillite) : the product of hydrothermal replacement of carbonate rocks in the Holy Cross Mts., Poland : a possible guide to ores

Nieć Marek, Pawlikowski Maciej

Geological Quarterly

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2019

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Vol. 63, No. 2

275--295

EN

The dolomites altered to dolomite-illitic rocks were foundac companying marcasite-pyrite-hematite mineralization within the Middle Devonian carbonate rocks in the eastern part of the Holy Cross Mts. (Poland) in the fault zones and their close vicinity. The alteration consist of dolomite recrystallization and replacement by illite, accompanied by small amounts of sillca, K-feldspars and disseminated pyrite or hematite. The final product of dolomite replacement by illite are massive, dolotmite-illitic rocks unevenly distributed within the unaltered dolomites or in fault breccia. They form irregular metric-sized nest-like bodies most often with blurred boundaries, or in some places sharp delineated veins and lenses. Illite crystallinity, demonstrates its hydrothermal origin. Altered rocks are characterized by elevated contents of REE, Rb, and sometimes other trace metal (Zr, Ti, Zn, U, Th, Ba and al.), compared to unaltered dolomites. The enrichment in REE, Zr and Ti implies their mobility in hydrothermal solutions. The lamprophyre intrusions present in the close vicinity may be considered as the probable source of potassium rich hydrothermal fluids. The peculiar features of dolomite-illitic rocks such as: their composition and occurrence close to the sulphide and hematite mineralization, allow supposing, that they may be a guide to deeply seated unknown ore deposits.