Carbon and oxygen isotope in situ analysis of calcite using secondary ion mass spectrometry in the Permian Kupferschiefer system, Saale subbasin, Eastern Germany
Cite as:
Mohammedyasin, Mohammed Seid; Magnall, Joseph M.; Gleeson, Sarah A.; Schulz, Hans-Martin; Scicchitano, Maria Rosa (2023): Carbon and oxygen isotope in situ analysis of calcite using secondary ion mass spectrometry in the Permian Kupferschiefer system, Saale subbasin, Eastern Germany. GFZ Data Services. https://doi.org/10.5880/GFZ.3.1.2023.003
Status
I N R E V I E W : Mohammedyasin, Mohammed Seid; Magnall, Joseph M.; Gleeson, Sarah A.; Schulz, Hans-Martin; Scicchitano, Maria Rosa (2023): Carbon and oxygen isotope in situ analysis of calcite using secondary ion mass spectrometry in the Permian Kupferschiefer system, Saale subbasin, Eastern Germany. GFZ Data Services. https://doi.org/10.5880/GFZ.3.1.2023.003
Abstract
The Kupferschiefer districts in Central Europe contain some of the world’s highest-grade sediment-hosted stratiform Cu (SSC) deposits (see Borg et al., 2012). The high-grade sulfide mineralization in the organic matter-rich marine mudstones of the Kupferschiefer (T1), and also in the underlying continental sandstones of the uppermost Rotliegend (S1) and overlying Zechstein Limestone (Ca1), in the Saale subbasin (Eastern Germany) are dominantly formed as a replacement of calcite cement (Mohammedyasin et al., 2023).
We provide carbonate major element chemistry, carbon isotope composition of organic matter, and calcite carbon and oxygen isotope microanalysis datasets of drill core samples from the Saale subbasin in Eastern Germany. The samples include the uppermost Rotliegend sandstone (S1), Kupferschiefer (T1) mudstones and lowermost Zechstein Limestone (Ca1), referred as the Kupferschiefer system, from three drill cores (Sangerhausen, Allstedt and Wallendorf).
For further details, see Mohammedyasin et al. (Chemical Geology, when available).
Authors
Mohammedyasin, Mohammed Seid;GFZ German Research Centre for Geosciences, Potsdam, Germany;Institute of Geological Sciences, Freie Universität Berlin, Berlin, Germany
Magnall, Joseph M.;GFZ German Research Centre for Geosciences, Potsdam, Germany
Gleeson, Sarah A.;GFZ German Research Centre for Geosciences, Potsdam, Germany;Institute of Geological Sciences, Freie Universität Berlin, Berlin, Germany
Schulz, Hans-Martin;GFZ German Research Centre for Geosciences, Potsdam, Germany
affiliation: GFZ German Research Centre for Geosciences, Potsdam, Germany
titles
title: Carbon and oxygen isotope in situ analysis of calcite using secondary ion mass spectrometry in the Permian Kupferschiefer system, Saale subbasin, Eastern Germany
publisher: GFZ Data Services
publicationYear: 2023
subjects
subject: Kupferschiefer
subject: Saale subbasin
subject: Eastern Germany
subject: Carbon isotopes
subject: Oxygen isotopes
subject: Secondary ion mass spectrometry
subject: Carbonate chemistry
subject: Seawater derived fluids
subject: Organic matter degradation
subject: Background variability
subject: Isotopic alteration haloes in calcite
subject: Mineralizing fluids
subject: Sediment hosted stratiform Cu (SSC) deposit
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CharacterString: The Kupferschiefer districts in Central Europe contain some of the world’s highest-grade sediment-hosted stratiform Cu (SSC) deposits (see Borg et al., 2012). The high-grade sulfide mineralization in the organic matter-rich marine mudstones of the Kupferschiefer (T1), and also in the underlying continental sandstones of the uppermost Rotliegend (S1) and overlying Zechstein Limestone (Ca1), in the Saale subbasin (Eastern Germany) are dominantly formed as a replacement of calcite cement (Mohammedyasin et al., 2023).
We provide carbonate major element chemistry, carbon isotope composition of organic matter, and calcite carbon and oxygen isotope microanalysis datasets of drill core samples from the Saale subbasin in Eastern Germany. The samples include the uppermost Rotliegend sandstone (S1), Kupferschiefer (T1) mudstones and lowermost Zechstein Limestone (Ca1), referred as the Kupferschiefer system, from three drill cores (Sangerhausen, Allstedt and Wallendorf).
For further details, see Mohammedyasin et al. (Chemical Geology, when available).
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