July 31, 2026 Dataset Open Access

Bachmann, Kai; Renno, Axel D.; Pospiech, Solveig; Duckstein, Alexandra

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    <dct:title>SEM-based automated mineralogy analysis of various granodiorite samples from the Kindisch quarry (Upper Lusatia, Germany)</dct:title>
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    <dcat:keyword>Granodiorite</dcat:keyword>
    <dcat:keyword>SEM-based automated mineralogy</dcat:keyword>
    <dcat:keyword>Kindisch</dcat:keyword>
    <dcat:keyword>Upper Lusatia</dcat:keyword>
    <dcat:keyword>Germany</dcat:keyword>
    <dcat:keyword>Mineral Liberation Analyser</dcat:keyword>
    <dcat:keyword>Lusatian Massif</dcat:keyword>
    <dct:issued rdf:datatype="http://www.w3.org/2001/XMLSchema#date">2026-07-31</dct:issued>
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    <dct:description>&lt;p&gt;SEM-based automated mineralogy was performed on polished thin sections from 20 different samples from the &amp;ldquo;Granittagebau Rauschwitz-Kindisch&amp;rdquo; (Upper Lusatia, Germany).&lt;/p&gt; &lt;p&gt;This quarry is frequently cited in geological literature as the &amp;ldquo;Kindisch Quarry&amp;rdquo; or &amp;ldquo;Steinbruch Kindisch.&amp;rdquo; The rocks are part of the Cadomian Lusatian Granodiorite Complex (Lusatian Massif).&lt;/p&gt; &lt;p&gt;The basement of the Lusatian Massif consists of monotonous, flysch-like, Precambrian greywacke and pelite sequences (Kr&amp;ouml;ner et al., 1994; Linnemann et al., 2010). These rocks are primarily found in the northern part of the massif and consolidated during the Cadomian orogeny (approximately 570&amp;ndash;540 million years ago).&amp;nbsp; The granodiorites and greywackes formed around 540&amp;ndash;530 Ma (Linnemann 2007; Tichomirowa et al. 2001; Tichomirowa 2002).&lt;/p&gt; &lt;p&gt;The samples were analyzed using a Mineral Liberation Analyzer (MLA) with SEM-based automated mineralogy at the Helmholtz Institute Freiberg for Resource Technology. The MLA consists of a FEI Quanta 650F field emission scanning electron microscope (SEM) with two Bruker Quantax X-Flash 5030 energy dispersive X-ray (EDX) detectors, as well as FEI&amp;#39;s MLA Suite v. 3.1.4.686 software for data acquisition. MLA identifies mineral grains based on backscattered electron (BSE) image segmentation and collection of EDX spectra of grains distinguished in BSE imaging mode. However, boundaries between two grains of the same mineral are not visible because their BSE intensities are identical.&amp;nbsp;The collected EDX spectra are then classified using a list of mineral spectra collected for granitic rocks and adapted to the mineralogical characteristics of the investigated granodiorites. More detailed information about the functionality of the MLA system can be found in Bachmann et al. (2017).&lt;/p&gt; &lt;p&gt;A resolution of 3&amp;times;3 &amp;micro;m per pixel was used. The measurements were taken during two measurement periods in December 2023 and January 2024 under identical conditions. The data are therefore summarized here and are not presented broken down by measurement date.&lt;/p&gt; &lt;p&gt;The data is structured as follows:&lt;/p&gt; &lt;ol&gt; &lt;li&gt;The main results are available as BMP images with a spatial resolution of 3 &amp;micro;m &amp;times; 3 &amp;micro;m per pixel.&lt;/li&gt; &lt;li&gt;The &lt;strong&gt;*_MINERAL_SAMPLE.bmp&lt;/strong&gt; files contain the assigned mineral information. The corresponding legend can be found in &lt;strong&gt;Granite_Legend.png&lt;/strong&gt;.&lt;/li&gt; &lt;li&gt;The &lt;strong&gt;*_BSE_SAMPLE.bmp&lt;/strong&gt; files contain the results of the backscattered electron contrast analysis as grayscale values.&lt;/li&gt; &lt;li&gt;The &amp;ldquo;&lt;strong&gt;Samples&lt;/strong&gt;&amp;rdquo; folder contains the original measurement data for each individual sample, along with the GXMAP data compiled for each sample in the &amp;lsquo;&lt;strong&gt;GXMAP&lt;/strong&gt;&amp;rsquo; subfolder, including the time of measurement.&lt;/li&gt; &lt;li&gt;The &amp;ldquo;&lt;strong&gt;Processing Scripts&lt;/strong&gt;&amp;rdquo; folder documents the individual scripts used in the automated workflows.&lt;/li&gt; &lt;li&gt;The &amp;ldquo;&lt;strong&gt;Mineral_List&amp;rdquo;&lt;/strong&gt; folder contains the adapted mineral list that was used.&lt;/li&gt; &lt;/ol&gt; &lt;p&gt;&amp;nbsp;&lt;/p&gt;</dct:description>
    <dct:description xml:lang="">The data is compiled into a single ZIP file.</dct:description>
    <dct:description xml:lang="">{"references": ["Tichomirowa M, Berger HJ, Koch EA, Belyatski B, G\u00f6tze J, Kempe U, Nasdala L, Schaltegger U (2001) Zircon ages of high-grade gneisses in the Eastern Erzgebirge (Central European Variscides)\u2014Constraints on origin of the rocks and Precambrian to Ordovician magmatic events in the Variscan foldbelt. Lithos 56:303\u2013332; https://doi.org/10.1016/S0024-4937(00)00066-9", "Tichomirowa M (2002) Zircon inheritance in diatexite granodiorites and its consequence on geochronology\u2014a case study in Lusatia and the Erzgebirge (Saxo-Thuringia, Eastern Germany). Chem Geol 191:209\u2013224; https://doi.org/10.1016/S0009-2541(02)00157-2", "Abdelfadil K, Romer RL, Seifert T, Lobst R (2013) Calc-alkaline lamprophyres from Lusatia (Germany)\u2014evidence for a repeatedly enriched mantle source. Chem Geol 353:230\u2013245 Article Google Scholar Arthaud F, Matte P (1977) Late Paleozoic strike-slip faulting in southern Europe and northern Africa: Result of a right-lateral shear zone between the Appalachian and the Urals. Geol Soc Am Bull 88:1305\u20131320 Article Google Scholar Barbarin B (2005) Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith, California: nature, origin, and relations with the hosts. Lithos 80:155\u2013177 Article Google Scholar Barthel M, Eichler B, Reichel W (2010) The Lower Permian (Rotliegend) flora of the Weissig Basin. J Cent Eur Geol 56(2):159\u2013192 Google Scholar Le Bas MJ, Le Maitre RW, Streckeisen A, Zanettin B, IUGS Subcommission on the Systematics of Igenous Rocks (1986) A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram. J Petrol 27(3):745\u2013750 Bia\u0142ek D, Kryza R, Oberc-Dziedzic T, Pin C (2014) Cambrian Zawid\u00f3w granodiorite in the Cadomian Lusatian Massif (Central European Variscides): what do the SHRIMP zircon ages mean? J Geosci 59:313\u2013326 Article Google Scholar Black LP, Kamo SL, Allen CM, Aleinikoff JN, Davies DW, Korsch RJ, Foudoulis C (2003) TEMORA 1: a new zircon standard for Phanerozoic U\u2013Pb geochronology. Chem Geol 200:155\u2013170 Article Google Scholar Black LP, Kamo SL, Allen CM, Davis DW, Aleinikoff JN, Valley JW, Mundil R, Campbell IH, Korsch RJ, Williams IS, Foudoulis C (2004) Improved 206Pb/238U microprobe geochronology by the monitoring of a trace-element \u2013related matrix effect; SHRIMP, ID\u2013TIMS, ELA\u2013ICP\u2013MS and oxygen isotope documentation for a series of zircon standards. Chem Geol 205:115\u2013140 Article Google Scholar Bowring J. F., McLean N. M., Bowring S. A. (2011) Engineering cyber infrastructure for U\u2013Pb geochronology: Tripoli and U\u2013Pb_Redux, Geochem Geophys Geosys 12(6): Q0AA19 Breitkreuz C, K\u00e4\u00dfner A, Tichomirowa M, Lapp M, Huang S, Stanek K (2021) The Late Carboniferous deeply eroded Tharandt Forest Caldera-Niederbobritzsch Granite Complex: A post-Variscan long-standing magmatic system in central Europe, Int J Earth Sci, online Ch\u00e1b J, Str\u00e1nik Z, Eli\u00e1\u0161 M (2007) Geological map of the Czech Republic 1: 500,000. Czech Geological Survey, Prague Chappell BW, White AJR (2001) Two contrasting granite types: 25 years later. Aust JEarth Sci 48:489\u2013499 Article Google Scholar Chen R-X, Zheng Y-F (2017) Metamorphic zirconology of continental subduction zones. J Asian Earth Sci 145:149\u2013176 Article Google Scholar Condon DJ, Schoene B, McLean NM, Bowring SA, Parrish RR (2015) Metrology and traceability of U\u2013Pb isotope dilution geochronology (EARTHTIME Tracer Calibration Part I). Geochim Cosmochim Acta 164:464\u2013480 Article Google Scholar DePaolo DJ (1981) Neodymium isotopes in the colorado front range and crust\u2013mantle evolution in the proterozoic. Nature 291:193\u2013196 Article Google Scholar Duthou JL, Couturie JP, Mierzejewski MP, Pin C (1991) Next dating of granite sample from the Karkonosze Mountains using Rb\u2013Sr total rock isochrone method. Przegla d Geologiczny 36:75\u201379 (in Polish, English summary) Edel JB, Schulmann K, Lexa O, Lardeaux JM (2018) Late Palaeozoic palaeomagnetic and tectonic constraints for amalgamation of Pangea supercontinent in the European Variscan Belt. Earth-Sci Rev 177:589\u2013612 Article Google Scholar Eidam J, G\u00f6tze J (1991) The granitic massif of K\u00f6nigshain\u2013Arnsdorf (Lusatian Anticlinal Zone): an example of a reversly zoned pluton. 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Lithos 80:155\u2013177 Article Google Scholar Barthel M, Eichler B, Reichel W (2010) The Lower Permian (Rotliegend) flora of the Weissig Basin. J Cent Eur Geol 56(2):159\u2013192 Google Scholar Le Bas MJ, Le Maitre RW, Streckeisen A, Zanettin B, IUGS Subcommission on the Systematics of Igenous Rocks (1986) A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram. J Petrol 27(3):745\u2013750 Bia\u0142ek D, Kryza R, Oberc-Dziedzic T, Pin C (2014) Cambrian Zawid\u00f3w granodiorite in the Cadomian Lusatian Massif (Central European Variscides): what do the SHRIMP zircon ages mean? J Geosci 59:313\u2013326 Article Google Scholar Black LP, Kamo SL, Allen CM, Aleinikoff JN, Davies DW, Korsch RJ, Foudoulis C (2003) TEMORA 1: a new zircon standard for Phanerozoic U\u2013Pb geochronology. Chem Geol 200:155\u2013170 Article Google Scholar Black LP, Kamo SL, Allen CM, Davis DW, Aleinikoff JN, Valley JW, Mundil R, Campbell IH, Korsch RJ, Williams IS, Foudoulis C (2004) Improved 206Pb/238U microprobe geochronology by the monitoring of a trace-element \u2013related matrix effect; SHRIMP, ID\u2013TIMS, ELA\u2013ICP\u2013MS and oxygen isotope documentation for a series of zircon standards. Chem Geol 205:115\u2013140 Article Google Scholar Bowring J. F., McLean N. M., Bowring S. A. (2011) Engineering cyber infrastructure for U\u2013Pb geochronology: Tripoli and U\u2013Pb_Redux, Geochem Geophys Geosys 12(6): Q0AA19 Breitkreuz C, K\u00e4\u00dfner A, Tichomirowa M, Lapp M, Huang S, Stanek K (2021) The Late Carboniferous deeply eroded Tharandt Forest Caldera-Niederbobritzsch Granite Complex: A post-Variscan long-standing magmatic system in central Europe, Int J Earth Sci, online Ch\u00e1b J, Str\u00e1nik Z, Eli\u00e1\u0161 M (2007) Geological map of the Czech Republic 1: 500,000. 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