July 31, 2026 Dataset Open Access

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

MARC21 XML Export

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    <subfield code="x">Tichomirowa M, Berger HJ, Koch EA, Belyatski B, Götze J, Kempe U, Nasdala L, Schaltegger U (2001) Zircon ages of high-grade gneisses in the Eastern Erzgebirge (Central European Variscides)—Constraints on origin of the rocks and Precambrian to Ordovician magmatic events in the Variscan foldbelt. Lithos 56:303–332; https://doi.org/10.1016/S0024-4937(00)00066-9</subfield>
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    <subfield code="x">Abdelfadil K, Romer RL, Seifert T, Lobst R (2013) Calc-alkaline lamprophyres from Lusatia (Germany)—evidence for a repeatedly enriched mantle source. Chem Geol 353:230–245      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 88:1305–1320      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 80:155–177      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):159–192      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):745–750      Białek D, Kryza R, Oberc-Dziedzic T, Pin C (2014) Cambrian Zawidów granodiorite in the Cadomian Lusatian Massif (Central European Variscides): what do the SHRIMP zircon ages mean? J Geosci 59:313–326      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–Pb geochronology. Chem Geol 200:155–170      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 –related matrix effect; SHRIMP, ID–TIMS, ELA–ICP–MS and oxygen isotope documentation for a series of zircon standards. Chem Geol 205:115–140      Article  Google Scholar       Bowring J. F., McLean N. M., Bowring S. A. (2011) Engineering cyber infrastructure for U–Pb geochronology: Tripoli and U–Pb_Redux, Geochem Geophys Geosys 12(6): Q0AA19      Breitkreuz C, Käßner 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      Cháb J, Stránik Z, Eliáš 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 48:489–499      Article  Google Scholar       Chen R-X, Zheng Y-F (2017) Metamorphic zirconology of continental subduction zones. J Asian Earth Sci 145:149–176      Article  Google Scholar       Condon DJ, Schoene B, McLean NM, Bowring SA, Parrish RR (2015) Metrology and traceability of U–Pb isotope dilution geochronology (EARTHTIME Tracer Calibration Part I). Geochim Cosmochim Acta 164:464–480      Article  Google Scholar       DePaolo DJ (1981) Neodymium isotopes in the colorado front range and crust–mantle evolution in the proterozoic. Nature 291:193–196      Article  Google Scholar       Duthou JL, Couturie JP, Mierzejewski MP, Pin C (1991) Next dating of granite sample from the Karkonosze Mountains using Rb–Sr total rock isochrone method. Przegla d Geologiczny 36:75–79 (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 177:589–612      Article  Google Scholar       Eidam J, Götze J (1991) The granitic massif of Königshain–Arnsdorf (Lusatian Anticlinal Zone): an example of a reversly zoned pluton. Chem Erde 51:55–71      Google Scholar       Eidam J, Hammer J, Korich D, Bielicki K-H (1995) Characterization, distribution and genesis of amphibole-bearing variscan granites in the lusatian granodiorite Massif (Northern margin of the Bohemian Massif). Neues Jahrb Mineral Abhandlungen 168:259–281      Google Scholar       Elter FM, Gaggero L, Mantovani F, Pandeli E, Costamagna LG (2020) The Atlas-East Variscan –Elbe shear system and its role in the formation of the pull-apart Late-Palaeozoic basins. Int J Earth Sci 109:739–760      Article  Google Scholar       Farina F, Stevens G, Gerdes A, Frei D (2014) Small-scale Hf isotopic variability in the Peninsula pluton (South Africa): the processes that control inheritance of source 176Hf/177Hf diversity in S-type granites. Contrib Mineral Petrol 168:1–18      Article  Google Scholar       Förster H-J, Romer RL (2010) Carboniferous magmatism. In: Linnemann U, Romer RL (eds) Pre-Mesozoic Geology of Saxo-Thuringia—from the cadomian active margin to the variscan orogen. Schweizerbart, Stuttgart, pp 287–308      Google Scholar       Förster H-J, Tischendorf G, Trumbull RB, Gottesmann B (1999) Late-collisional granites in the variscan erzgebirge. Germany J Petrol 40(11):1613–1645      Article  Google Scholar       Förster H-J, Rhede D, Stein HJ, Romer RL, Tischendorf G (2012) Paired uraninite and molybdenite dating oft he Königshain granite: implications fort he onset of late-Variscan magmatism in the Lausitz Block. Int J Earth Sci 101:57–67      Article  Google Scholar       Friedl G, Finger F, Paquette J-L, von Quadt A, McNaughton NJ, Fletcher IR (2004) Pre-variscan geological events in the austrian part of the bohemian massif deduced from U–Pb zircon ages. Int J Earth Sci 93:802–823      Article  Google Scholar       Gerdes A, Zeh A (2006) Combined U–Pb and Hf isotope LA-(MC)ICP-MS analyses of detrital zircons: Comparison with SHRIMP and new constraints for the provenance and age of an Armorican metasediment in Central Germany. EarthPlanet Sci Lett 249:47–61      Article  Google Scholar       Gerstenberger H, Haase G (1997) A highly effective emitter substance for mass spectrometric Pb isotope ratio determinations. Chem Geol 136:309–312      Article  Google Scholar       Geyer G, Buschmann B, Elicki O (2014) A new lowermost middle Cambiran (Series 3, Stage 5) faunule from Saxony (Germany) and its bearing on the tectonostratigraphic history of the Saxothuringian domain. Paläontol Z 88:239–262      Article  Google Scholar       Hammer J (1996) Geochemie und Petrogenese der cadomischen und spätvariszischen Granitoide der Lausitz. Freib Forsch C463:1–107      Google Scholar       Hammer J, Eidam J, Röber B, Ehling B-C (1999) Prävariscischer und variscischer granitoider Magmatismus am NE-Rand des Böhmischen Massivs–Geochemie und Petrogenese. Z Geol Wiss 27(5/6):401–415      Google Scholar       Hecht L, Thuro K, Plinninger R, Cuney M (1999) Mineralogical and geochemical characteristics of hydrothermal alteration and episyenitization in the Königshain granites, northern Bohemian Massif, Germany. Int J Earth Sci 88:236–252      Article  Google Scholar       Heinonen A, Anderson T, Rämö T, Whitehouse M (2015) The source of Proterozoic anorthosite and rapakivi granite magmatism: evidence from combined in situ Hf-O isotopes of zircon in the Ahvenisto complex, southeastern Finland. J Geol Soc 172:103–112      Article  Google Scholar       Hintze JL, Nelson RD (1998) Violin plots: a box plot-density trace synergism. Am Stat 52(2):181–184      Google Scholar       Hoffmann U, Breitkreuz C, Breiter K, Sergeev S, Stanek K, Tichomirowa M (2013) Carboniferous-Permian volcanic evolution in Central Europe—U/Pb ages of volcanic rocks in Saxony (Germany) and northern Bohemia (Czech Republic). Int J Earth Sci 102:73–99      Article  Google Scholar       Hofmann M, Linnemann U, Gerdes A, Ullrich B, Schauer M (2009) Timing of dextral strike-slip processes and basement exhumation in the Elbe Zone (Saxo-Thuringian Zone): the final pulse of the Variscan Orogeny in the Bohemian Massif constrained by LA–SF–ICP–MS U–Pb zircon data. In: Murphy JB, Keppie JD, Hynes AJ (eds.) Ancient Orogens and Modern Analogues. Geol Soc SpecPubl 327:197–214      Horstwood MSA, Košler J, Gehrels G, Jackson SE, McLean NM, Paton C, Pearson NJ, Sircombe K, Sylevester P, Vermeesch P, Bowring JF, Condon DJ, Schoene B (2016) Community-derived standards for LA–ICP–MS U-(Th-)Pb geochronology—uncertainty propagation, age interpretation and data reporting. Geostand Geoanalytical Res 40(3):311–332      Article  Google Scholar       Huhle K, Lange J-M (2010) Über ein vorkommen von permosiles im untergrund des schlosses wackerbarth in radebeul (Sachsen). J CentEur Geol 56(2):127–136      Google Scholar       Jung S, Pfänder JA (2007) Source composition and melting temperatures of orogenic granitoids: constraints from CaO/Na2O, Al2O3/TiO2 and accessory mineral saturation thermometry. Eur J Mineral 19:859–870      Article  Google Scholar       Kindermann A, Fiedler F, Seifert T, Uhlig S (2003) Platinmetall-Führung der Ni–Cu-Sulfidmineralisationen im Bereich der Lausitzer Antiklinalzone. Z AngewGeol 49:43–47      Google Scholar       Kober B (1987) Single zircon evaporation combined with Pb+ emitter bedding for 207Pb/206Pb-age investigations using thermal ion mass spectrometry, and implications for zirconology. Contrib Mineral Petrol 96:63–71      Article  Google Scholar       Kozdrój W, Krentz O, Opletal M (2001) Geological Map and Comments on the Geological Map Lausitz, Jizera, Karkonosze (without Cenozoic sediments) 1:100000. Państwowy Instytut Geologiczny, Warsaw.      Kramer W, Müller B, Peschel A (1977) Zur tektonischen und substantiellen Charakteristik der Basite des Lausitzer Antiklinoriums und deren Altersbeziehung. Z Geol Wiss 5:95–100      Google Scholar       Kröner A, Willner AP (1998) Time of formation and peak of Variscan HP-HT metamorphism of quartz-feldspar rocks in the central Erzgebirge, Saxony, Germany. Contrib Mineral Petrol 132:1–20      Article  Google Scholar       Kröner A, Hegner E, Hammer J, Haase G, Bielicki K-H, Krauss M, Eidam J (1994) Geochronology and Nd-Sr systematics of Lusatian granitoids: significance for the evolution of the Variscan orogeny in east-central Europe. Geol Rdsch 83:357–376; https://doi.org/10.1007/BF00210551</subfield>
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    <subfield code="x">Abdelfadil K, Romer RL, Seifert T, Lobst R (2013) Calc-alkaline lamprophyres from Lusatia (Germany)—evidence for a repeatedly enriched mantle source. Chem Geol 353:230–245      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 88:1305–1320      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 80:155–177      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):159–192      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):745–750      Białek D, Kryza R, Oberc-Dziedzic T, Pin C (2014) Cambrian Zawidów granodiorite in the Cadomian Lusatian Massif (Central European Variscides): what do the SHRIMP zircon ages mean? J Geosci 59:313–326      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–Pb geochronology. Chem Geol 200:155–170      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 –related matrix effect; SHRIMP, ID–TIMS, ELA–ICP–MS and oxygen isotope documentation for a series of zircon standards. Chem Geol 205:115–140      Article  Google Scholar       Bowring J. F., McLean N. M., Bowring S. A. (2011) Engineering cyber infrastructure for U–Pb geochronology: Tripoli and U–Pb_Redux, Geochem Geophys Geosys 12(6): Q0AA19      Breitkreuz C, Käßner 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      Cháb J, Stránik Z, Eliáš 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 48:489–499      Article  Google Scholar       Chen R-X, Zheng Y-F (2017) Metamorphic zirconology of continental subduction zones. J Asian Earth Sci 145:149–176      Article  Google Scholar       Condon DJ, Schoene B, McLean NM, Bowring SA, Parrish RR (2015) Metrology and traceability of U–Pb isotope dilution geochronology (EARTHTIME Tracer Calibration Part I). Geochim Cosmochim Acta 164:464–480      Article  Google Scholar       DePaolo DJ (1981) Neodymium isotopes in the colorado front range and crust–mantle evolution in the proterozoic. Nature 291:193–196      Article  Google Scholar       Duthou JL, Couturie JP, Mierzejewski MP, Pin C (1991) Next dating of granite sample from the Karkonosze Mountains using Rb–Sr total rock isochrone method. Przegla d Geologiczny 36:75–79 (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 177:589–612      Article  Google Scholar       Eidam J, Götze J (1991) The granitic massif of Königshain–Arnsdorf (Lusatian Anticlinal Zone): an example of a reversly zoned pluton. Chem Erde 51:55–71      Google Scholar       Eidam J, Hammer J, Korich D, Bielicki K-H (1995) Characterization, distribution and genesis of amphibole-bearing variscan granites in the lusatian granodiorite Massif (Northern margin of the Bohemian Massif). Neues Jahrb Mineral Abhandlungen 168:259–281      Google Scholar       Elter FM, Gaggero L, Mantovani F, Pandeli E, Costamagna LG (2020) The Atlas-East Variscan –Elbe shear system and its role in the formation of the pull-apart Late-Palaeozoic basins. Int J Earth Sci 109:739–760      Article  Google Scholar       Farina F, Stevens G, Gerdes A, Frei D (2014) Small-scale Hf isotopic variability in the Peninsula pluton (South Africa): the processes that control inheritance of source 176Hf/177Hf diversity in S-type granites. Contrib Mineral Petrol 168:1–18      Article  Google Scholar       Förster H-J, Romer RL (2010) Carboniferous magmatism. In: Linnemann U, Romer RL (eds) Pre-Mesozoic Geology of Saxo-Thuringia—from the cadomian active margin to the variscan orogen. Schweizerbart, Stuttgart, pp 287–308      Google Scholar       Förster H-J, Tischendorf G, Trumbull RB, Gottesmann B (1999) Late-collisional granites in the variscan erzgebirge. Germany J Petrol 40(11):1613–1645      Article  Google Scholar       Förster H-J, Rhede D, Stein HJ, Romer RL, Tischendorf G (2012) Paired uraninite and molybdenite dating oft he Königshain granite: implications fort he onset of late-Variscan magmatism in the Lausitz Block. Int J Earth Sci 101:57–67      Article  Google Scholar       Friedl G, Finger F, Paquette J-L, von Quadt A, McNaughton NJ, Fletcher IR (2004) Pre-variscan geological events in the austrian part of the bohemian massif deduced from U–Pb zircon ages. Int J Earth Sci 93:802–823      Article  Google Scholar       Gerdes A, Zeh A (2006) Combined U–Pb and Hf isotope LA-(MC)ICP-MS analyses of detrital zircons: Comparison with SHRIMP and new constraints for the provenance and age of an Armorican metasediment in Central Germany. EarthPlanet Sci Lett 249:47–61      Article  Google Scholar       Gerstenberger H, Haase G (1997) A highly effective emitter substance for mass spectrometric Pb isotope ratio determinations. Chem Geol 136:309–312      Article  Google Scholar       Geyer G, Buschmann B, Elicki O (2014) A new lowermost middle Cambiran (Series 3, Stage 5) faunule from Saxony (Germany) and its bearing on the tectonostratigraphic history of the Saxothuringian domain. Paläontol Z 88:239–262      Article  Google Scholar       Hammer J (1996) Geochemie und Petrogenese der cadomischen und spätvariszischen Granitoide der Lausitz. Freib Forsch C463:1–107      Google Scholar       Hammer J, Eidam J, Röber B, Ehling B-C (1999) Prävariscischer und variscischer granitoider Magmatismus am NE-Rand des Böhmischen Massivs–Geochemie und Petrogenese. Z Geol Wiss 27(5/6):401–415      Google Scholar       Hecht L, Thuro K, Plinninger R, Cuney M (1999) Mineralogical and geochemical characteristics of hydrothermal alteration and episyenitization in the Königshain granites, northern Bohemian Massif, Germany. Int J Earth Sci 88:236–252      Article  Google Scholar       Heinonen A, Anderson T, Rämö T, Whitehouse M (2015) The source of Proterozoic anorthosite and rapakivi granite magmatism: evidence from combined in situ Hf-O isotopes of zircon in the Ahvenisto complex, southeastern Finland. J Geol Soc 172:103–112      Article  Google Scholar       Hintze JL, Nelson RD (1998) Violin plots: a box plot-density trace synergism. Am Stat 52(2):181–184      Google Scholar       Hoffmann U, Breitkreuz C, Breiter K, Sergeev S, Stanek K, Tichomirowa M (2013) Carboniferous-Permian volcanic evolution in Central Europe—U/Pb ages of volcanic rocks in Saxony (Germany) and northern Bohemia (Czech Republic). Int J Earth Sci 102:73–99      Article  Google Scholar       Hofmann M, Linnemann U, Gerdes A, Ullrich B, Schauer M (2009) Timing of dextral strike-slip processes and basement exhumation in the Elbe Zone (Saxo-Thuringian Zone): the final pulse of the Variscan Orogeny in the Bohemian Massif constrained by LA–SF–ICP–MS U–Pb zircon data. In: Murphy JB, Keppie JD, Hynes AJ (eds.) Ancient Orogens and Modern Analogues. Geol Soc SpecPubl 327:197–214      Horstwood MSA, Košler J, Gehrels G, Jackson SE, McLean NM, Paton C, Pearson NJ, Sircombe K, Sylevester P, Vermeesch P, Bowring JF, Condon DJ, Schoene B (2016) Community-derived standards for LA–ICP–MS U-(Th-)Pb geochronology—uncertainty propagation, age interpretation and data reporting. Geostand Geoanalytical Res 40(3):311–332      Article  Google Scholar       Huhle K, Lange J-M (2010) Über ein vorkommen von permosiles im untergrund des schlosses wackerbarth in radebeul (Sachsen). J CentEur Geol 56(2):127–136      Google Scholar       Jung S, Pfänder JA (2007) Source composition and melting temperatures of orogenic granitoids: constraints from CaO/Na2O, Al2O3/TiO2 and accessory mineral saturation thermometry. Eur J Mineral 19:859–870      Article  Google Scholar       Kindermann A, Fiedler F, Seifert T, Uhlig S (2003) Platinmetall-Führung der Ni–Cu-Sulfidmineralisationen im Bereich der Lausitzer Antiklinalzone. Z AngewGeol 49:43–47      Google Scholar       Kober B (1987) Single zircon evaporation combined with Pb+ emitter bedding for 207Pb/206Pb-age investigations using thermal ion mass spectrometry, and implications for zirconology. Contrib Mineral Petrol 96:63–71      Article  Google Scholar       Kozdrój W, Krentz O, Opletal M (2001) Geological Map and Comments on the Geological Map Lausitz, Jizera, Karkonosze (without Cenozoic sediments) 1:100000. Państwowy Instytut Geologiczny, Warsaw.      Kramer W, Müller B, Peschel A (1977) Zur tektonischen und substantiellen Charakteristik der Basite des Lausitzer Antiklinoriums und deren Altersbeziehung. Z Geol Wiss 5:95–100      Google Scholar       Kröner A, Willner AP (1998) Time of formation and peak of Variscan HP-HT metamorphism of quartz-feldspar rocks in the central Erzgebirge, Saxony, Germany. Contrib Mineral Petrol 132:1–20      Article  Google Scholar       Kröner A, Hegner E, Hammer J, Haase G, Bielicki K-H, Krauss M, Eidam J (1994) Geochronology and Nd-Sr systematics of Lusatian granitoids: significance for the evolution of the Variscan orogeny in east-central Europe. Geol Rdsch 83:357–376     Return to ref 1994 in article      Article  Google Scholar       Kroner U, Hahn T, Romer RL, Linnemann U (2007) The Variscan orogeny in the Saxo-Thuringian zone—heterogenous overprint of Cadomian/Paleozoic Peri-Gondwana crust. In Linnemann U, Nance RD, Kraft P, Zulauf G (eds.) The evolution of the Rheic Ocean: From Avalonian-Cadomian Active Margin to Alleghenian-Variscan Collision. Geol Soc Am Spec 423:153–172      Kryza R, Schaltegger U, Oberc-Dziedzic T, Rin C, Ovtcharova M (2014a) Geochronology of a composite granitoid pluton: a high-precision ID–TIMS U–Pb zircon study of the Variscan Karkonosze Granite (SW Poland). 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    <subfield code="x">Linnemann U (2007) Ediacaran rocks from the Cadomian basement of the Saxo-Thuringian Zone (NE Bohemian Massif, Germany): age constraints, geotectonic setting and basin development. In: Vickers-Rich P, Komarower P (eds.) The Rise and Fall of the Ediacaran Biota, Geol Soc Spec Publ 286:35–51; https://doi.org/10.1144/SP286.4</subfield>
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    <subfield code="x">Bachmann , K. , Frenzel , M. , Krause , J. , and Gutzmer , J. , 2017 , Advanced Identification and Quantification of In-Bearing Minerals by Scanning Electron Microscope-Based Image Analysis : Microscopy and Microanalysis  , v. 23 , no. 3 , p.527 –537; https://doi.org/10.1017/S1431927617000460</subfield>
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    <subfield code="a">Renno, Axel D.</subfield>
    <subfield code="u">Helmholtz Zentrum Dresden Rossendorf, Helmholtz Institute Freiberg for Resource Technology</subfield>
    <subfield code="0">(orcid)0000-0002-8289-1059</subfield>
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    <subfield code="a">Pospiech, Solveig</subfield>
    <subfield code="u">Helmholtz-Zentrum Dresden-Rossendorf, Institute for Resource Ecology (IRE)</subfield>
    <subfield code="0">(orcid)0000-0003-2727-2375</subfield>
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    <subfield code="a">Duckstein, Alexandra</subfield>
    <subfield code="u">Helmholtz-Zentrum Dresden-Rossendorf, Institute for Resource Ecology (IRE)</subfield>
    <subfield code="0">(orcid)0009-0002-5241-8540</subfield>
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    <subfield code="a">&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;</subfield>
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    <subfield code="a">Bachmann, Kai</subfield>
    <subfield code="u">Helmholtz Zentrum Dresden Rossendorf, Helmholtz Institute Freiberg for Resource Technology</subfield>
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