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Journal articles on the topic 'Erzgebirge Erzgebirge'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Murdock, Caitlin E. "A Gulag in the Erzgebirge? Forced Labor, Political Legitimacy, and Eastern German Uranium Mining in the Early Cold War, 1946–1949." Central European History 47, no. 4 (December 2014): 791–821. http://dx.doi.org/10.1017/s0008938914001939.

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“Dear Papa! I have been conscripted into a living grave. . . .” So began a letter in the West Berlin newspaperDer Sozialdemokratin March 1948. The young man had been sent to work in the Soviet occupation zone's uranium mines, near Aue in the Saxon Erzgebirge (Ore Mountains), and had written to his parents in despair. The news article that accompanied the letter explained, “The uranium mines… are not in the Urals, but in the Erzgebirge. But reports from [the Erzgebirge] are as hard to come by as [ones] from the Urals.” Other newspapers in Germany's Western zones of occupation also published reports of “slave conditions,” and “forced labor” in the mines.

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2

Baumann, Martin. "Verbreitung vonLophozia obtusaim Erzgebirge." Herzogia 27, no. 1 (July 2014): 157–64. http://dx.doi.org/10.13158/heia.27.1.2014.157.

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3

Baumann, Martin. "Zum Vorkommen vonTayloria tenuisim Erzgebirge." Herzogia 24, no. 1 (June 2011): 103–19. http://dx.doi.org/10.13158/heia.24.1.2011.103.

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4

Horber, Matthias. "High-Tech-Lohnbeschichtung im Erzgebirge." JOT Journal für Oberflächentechnik 44, no. 2 (February 2004): 14–16. http://dx.doi.org/10.1007/bf03240821.

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5

Baumann, Martin. "Verbreitung und Soziologie vonAnastrepta orcadensisim Erzgebirge." Herzogia 25, no. 2 (December 2012): 245–70. http://dx.doi.org/10.13158/heia.25.2.2010.245.

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6

Pasche, Eckart. "Der Dollar stammt aus dem Erzgebirge." VDI nachrichten 74, no. 09 (2020): 27. http://dx.doi.org/10.51202/0042-1758-2020-09-27.

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7

MINGRAM, BIRGIT. "The Erzgebirge, Germany, a subducted part of northern Gondwana: geochemical evidence for repetition of early Palaeozoic metasedimentary sequences in metamorphic thrust units." Geological Magazine 135, no. 6 (November 1998): 785–801. http://dx.doi.org/10.1017/s0016756898001769.

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One of the major metamorphic terranes of the Bohemian Massif, the Erzgebirge, is interpreted to record a subducted part of a Palaeozoic margin of Gondwana. A geochemical study on non-calcareous metasediments from the various metamorphic units from lower greenschist to granulite facies metamorphism supports a recently established thrust model. Geochemical discrimination and correlation from the metasediments of the Erzgebirge suggest repetition of an early Palaeozoic metasedimentary sequence in metamorphic thrust units. This new finding is in line with recent radiometric dating of intercalated metarhyolitic rocks, which yielded ages of around 480 Ma. It is furthermore supported by correlation with a low-grade standard section in Thuringia, which represents the transition from an orogenic belt to a passive margin setting, with highly mature sediments. Significant geochemical signatures have been identified in three different lithotypes, which reappear in at least three metamorphic units of the Erzgebirge. Geochemical correlation of these units was established using simple comparison of averages and with statistical techniques. The identification of significant geochemical signatures from different lithotypes in metamorphic suites has important implications for terrane analysis and reconstruction of ancient tectonic settings.The repetition of lithologies and their distinct chemical compositions in progressively metamorphosed units is useful for examining element mobility during Barrovian metamorphism. Statistical comparison implies that Li is progressively depleted from the greenschist to amphibolite facies, whereas Ca exhibits some enrichment. All the other elements studied are considered to be immobile.

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8

Schmitt, Ulrich, and Werner Gunther. "Haamitland, mei Arzgebirg. Lieder aus dem Erzgebirge." Jahrbuch für Volksliedforschung 34 (1989): 232. http://dx.doi.org/10.2307/849278.

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9

Thieding, Hans-Wilhelm. "Fachexkursion in den Raum Zwickau im Erzgebirge." Wasser und Abfall 16, no. 9 (September 2014): 33–34. http://dx.doi.org/10.1365/s35152-014-0711-9.

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10

Schneider, Jörg W., Ronny Rößler, and Frank Fischer. "Rotliegend des Chemnitz-Beckens (syn. Erzgebirge-Becken)." Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 61 (October 25, 2012): 530–88. http://dx.doi.org/10.1127/sdgg/61/2012/530.

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11

Nebe, Wolfgang, and Mengistu Abiy. "Chemie von Quellwassern in bewaldeten Einzugsgebieten des Erzgebirges. Springwater Chemistry of Forested Water Catchment Areas in the Erzgebirge." Forstwissenschaftliches Centralblatt 121, no. 1 (February 2002): 1–14. http://dx.doi.org/10.1046/j.1439-0337.2002.01040.x.

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12

Woudhuizen, Fred C. "Towards a reconstruction of Tin-trade routes in mediterranean protohistory." Praehistorische Zeitschrift 92, no. 2 (March 27, 2018): 342–53. http://dx.doi.org/10.1515/pz-2017-0023.

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Zusammenfassung: In dieser Arbeit wird ein für die Bronzezeit des Mittelmeerraums grundlegendes Thema angesprochen: Woher stammt das Zinn zur Herstellung von Bronzeobjekten? Tatsächlich lassen sich nur zwei Möglichkeiten erkennen: der Mittlere Osten (Afghanistan und die Region Oxus an seiner nordöstlichen Grenze) oder der Westen (Erzgebirge, Bretagne, Cornwall oder Gallizien).

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13

Schmidt, Johann. "Wasserwirtschaftsplan zum Talsperren-System Mittleres Erzgebirge im Regelbetrieb." WASSERWIRTSCHAFT 110, no. 1 (January 2020): 28–33. http://dx.doi.org/10.1007/s35147-019-0321-2.

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14

Forster, H. J., G. Tischendorf, R. B. Trumbull, and B. Gottesmann. "Late-Collisional Granites in the Variscan Erzgebirge, Germany." Journal of Petrology 40, no. 11 (November 1, 1999): 1613–45. http://dx.doi.org/10.1093/petroj/40.11.1613.

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15

Tischendorf, G., and H. J. Förster. "Acid magmatism and related metallogenesis in the Erzgebirge." Geological Journal 25, no. 3-4 (July 1990): 443–54. http://dx.doi.org/10.1002/gj.3350250326.

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16

Seifert, Erhard, and Frank Müller. "Orthotrichum shawiiim Erzgebirge — Erstfund für Sachsen und Deutschland." Herzogia 30, no. 2 (December 2017): 343–52. http://dx.doi.org/10.13158/heia.30.2.2017.343.

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17

Massonne, H. J., and R. D. Neuser. "Ilmenite exsolution in olivine from the serpentinite body at Zöblitz, Saxonian Erzgebirge – microstructural evidence using EBSD." Mineralogical Magazine 69, no. 2 (April 2005): 119–24. http://dx.doi.org/10.1180/0026461056920239.

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AbstractIn the large serpentinite body at Zöblitz, which is part of the Gneiss-Eclogite Unit of the Saxonian Erzgebirge, ilmenite rods have been detected in olivine. Although these rods are ≤1 μm wide, they can be unequivocally identified as ilmenite using electron backscatter diffraction. We also applied this method to prove that ilmenite is topotactically intergrown with the olivine host ([100]ol ‖ [001]ilm). This relation was found previously, e.g. for ilmenite exsolved from olivine of garnet peridotite from Alpe Arami, Swiss Alps. The degree of this exsolution phenomenon in the Alpe Arami rocks was taken as an indication of the original formation of a Ti-bearing mineral at depths of ∽300 km. As in the olivines of the serpentinite from Zöblitz, the density of the ilmenite rods is significantly less than in the rock from Alpe Arami. We think that our observation is compatible with previous P-T estimates of close to 4 GPa and 1000–1100°C for the ultramafic bodies in the central Saxonian Erzgebirge.

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18

Küßner, Ralf, and Reinhard Mosandl. "Comparison of direct and indirect estimation of leaf area index in mature Norway spruce stands of eastern Germany." Canadian Journal of Forest Research 30, no. 3 (March 1, 2000): 440–47. http://dx.doi.org/10.1139/x99-227.

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IIn three mature Norway spruce (Picea abies (L.) Karst.) stands of the Erzgebirge (Ore Mountains) in eastern Germany, the performance of the LAI-2000 plant canopy analyzer (LI-COR instruments) was tested for indirect estimation of leaf area index (LAI). The LAI-2000 calculates effective leaf area index (LAIe, m2/m2) resulting from radiation measurements and subsequent model calculations. LAIe underestimated directly estimated half the total leaf area index (LAI0.5t, m2/m2) by 37-82% as determined from allometric relationships derived from subsample harvesting. The degree of underestimation was dependent upon stand density in two of three spruce stands examined; it was the highest in sparsely stocked plots. The relationship of LAIe to allometrically determined LAI0.5t for one of the three stands differed significantly from the other two spruce stands and the underestimation of LAI0.5t was less distinct. This was explained by stand structure, i.e., higher amounts of nonassimilating surfaces relative to LAI0.5t. These results indicate that the LAI-2000 is not generally applicable for estimation of LAI in mature spruce stands of the Erzgebirge because of effects of stand structure on LAIe-LAI0.5t relationships, which are stand specific.

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19

Friedolin Lingg, Andreas. "Schools of Empiricism." Jahrbuch für Wirtschaftsgeschichte / Economic History Yearbook 62, no. 1 (April 30, 2021): 261–89. http://dx.doi.org/10.1515/jbwg-2021-0010.

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Abstract Recent research emphasizes that empiricist approaches already emerged long before the seventeenth and eighteenth century. While many of these contributions focus on specific professions, it is the aim of this article to supplement this discourse by describing certain social spaces that fostered empiricist attitudes. A particularly interesting example in this respect is the mining region of the Erzgebirge (Saxony) in the fifteenth and sixteenth century. The following article will use this mining district as a kind of historical laboratory, as a space not only for scientific observation but also as a structure within which specific forms of knowledge were socially tested, to show how the economic transformation of this region supported the rise of characteristic elements of empiricist thinking. It is common practice to link the appraisal of useful knowledge, (personal) experience and the distrust towards (scholastic) authorities in those days with only small minorities. By addressing not only the struggles of the commercial elites but also the challenges faced by the average resident of a mining town, this paper tries to add to this view by demonstrating how entire masses of people inhabiting the late medieval Erzgebirge were affected by and schooled to think in empiricist ways.

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20

Lapp, Manuel, and Christoph Breitkreuz. "The Late Paleozoic volcanic centers in the eastern Erzgebirge." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 97 (March 11, 2015): 143–68. http://dx.doi.org/10.1127/jmogv/97/0007.

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21

Stams, D., and H. Gerstenberger. "Uranium Mapping of a Zircon Crystal from Erzgebirge Granites." Isotopenpraxis Isotopes in Environmental and Health Studies 27, no. 6 (January 1991): 299–301. http://dx.doi.org/10.1080/10256019108622547.

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22

Perchuk, A. L. "Melt inclusions in garnet from diamondiferous gneiss, Erzgebirge, Germany." Doklady Earth Sciences 421, no. 1 (July 2008): 832–34. http://dx.doi.org/10.1134/s1028334x08050279.

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23

THALHEIM, KLAUS. "THE 1477 SILVER FIND AT THE ST. GEORG MINE IN SCHNEEBERG AND SIGNIFICANT ORE SPECIMENS IN THE MUSEUM OF MINERALOGY AND GEOLOGY IN DRESDEN." Earth Sciences History 38, no. 2 (November 1, 2019): 157–72. http://dx.doi.org/10.17704/1944-6178-38.2.157.

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ABSTRACT Two silver ore specimens in the mineralogical collection of the Senckenberg Natural History Collections Dresden, Museum of Mineralogy and Geology, are samples from one of the most spectacular silver finds in Saxon Erzgebirge. The history of the find and of the two silver ore specimens is discussed. The origin of such a rich deposit of silver ore is examined in relationship to the geology of mineral deposits.

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24

Schmädicke, Esther, and Jürgen Gose. "Water transport by subduction: Clues from garnet of Erzgebirge UHP eclogite." American Mineralogist 102, no. 5 (May 1, 2017): 975–86. http://dx.doi.org/10.2138/am-2017-5920.

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Abstract A key question concerning the water budget of Earth’s mantle is how much water is actually recycled into the mantle by the subduction of eclogitized oceanic crust. Hydrous phases are stable only in quartz eclogite not coesite eclogite so that water transport to greater depths is mainly governed by structural water in omphacite and garnet. Here we explore if garnet can be used as a proxy to assess the amount of this water. Available data on the water contents of garnet in coesite eclogite vary over orders of magnitude, from a few up to ca. 2000 ppm. By implication, the maximum bulk-rock water contents are unrealistically high (wt% level). New data from the Erzgebirge indicate moderate amounts of structural H2O stored in garnet (43–84 ppm), omphacite (400–820 ppm), and in the bulk coesite eclogite (ca. 280–460 ppm). Higher garnet water contents occur, but these are not primary features. They are related to molecular water in fluid inclusions that can be attributed to eclogite-facies fluid influx postdating the metamorphic peak. Fluid influx also caused the uptake of additional structural water in garnet domains close to fluid inclusions. Such secondary H2O incorporation is only possible in the case of primary water-deficiency indicating that garnet hosted less water than it was able to store. This is insofar astonishing as comparably high H2O amounts are liberated by the breakdown of prograde eclogite-facies hydrous minerals as a result of ultrahigh-pressure (UHP) metamorphism. Judging from Erzgebirge quartz eclogite, dehydration of 5–10% hydrous minerals (±equal portions of zoisite+calcic amphibole) produces 1500–3000 ppm water. We infer that the largest part of the liberated water escaped, probably due to kinetic reasons, and hydrated exhuming UHP slices in the hanging-wall. Depending on the physical conditions, water influx in eclogite during exhumation (1) produces fluid inclusions and simultaneously enhances the structural water content of nominally anhydrous minerals—as in the Erzgebirge—and/or (2) it may give rise to retrograde hydrous minerals. We conclude that eclogite transports moderate quantities of water (several hundred parts per million) to mantle depths beyond 100 km, an amount equivalent to that in ca. 1% calcic amphibole.

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25

Tichomirowa, Marion, Axel Gerdes, Manuel Lapp, Dietmar Leonhardt, and Martin Whitehouse. "The Chemical Evolution from Older (323–318 Ma) towards Younger Highly Evolved Tin Granites (315–314 Ma)—Sources and Metal Enrichment in Variscan Granites of the Western Erzgebirge (Central European Variscides, Germany)." Minerals 9, no. 12 (December 11, 2019): 769. http://dx.doi.org/10.3390/min9120769.

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The sources and critical enrichment processes for granite related tin ores are still not well understood. The Erzgebirge represents one of the classical regions for tin mineralization. We investigated the four largest plutons from the Western Erzgebirge (Germany) for the geochemistry of bulk rocks and autocrystic zircons and relate this information to their intrusion ages. The source rocks of the Variscan granites were identified as high-grade metamorphic rocks based on the comparison of Hf-O isotope data on zircons, the abundance of xenocrystic zircon ages as well as Nd and Hf model ages. Among these rocks, restite is the most likely candidate for later Variscan melts. Based on the evolution with time, we could reconstruct enrichment factors for tin and tungsten starting from the protoliths (575 Ma) that were later converted to high-grade metamorphic rocks (340 Ma) and served as sources for the older biotite granites (323–318 Ma) and the tin granites (315–314 Ma). This evolution involved a continuous enrichment of both tin and tungsten with an enrichment factor of ~15 for tin and ~7 for tungsten compared to the upper continental crust (UCC). Ore level concentrations (>10–100 times enrichment) were achieved only in the greisen bodies and dykes by subsequent hydrothermal processes.

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26

Gottesmann, Bärbel, and Hans-Jürgen Förster. "Sekaninaite from the Satzung granite (Erzgebirge, Germany): magmatic or xenolithic?" European Journal of Mineralogy 16, no. 3 (June 7, 2004): 483–91. http://dx.doi.org/10.1127/0935-1221/2004/0016-0483.

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27

Schneider, Jörg W., Klaus Hoth, Birgit G. Gaitzsch, Hans J. Berger, Henry Steinborn, Harald Walter, and Matthias K. Zeidler. "Carboniferous stratigraphy and development of the Erzgebirge Basin, East Germany." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 156, no. 3 (September 1, 2005): 431–66. http://dx.doi.org/10.1127/1860-1804/2005/0156-0431.

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28

Schmädicke, Esther. "Quartz pseudomorphs after coesite in eclogites from the Saxonian Erzgebirge." European Journal of Mineralogy 3, no. 2 (April 18, 1991): 231–38. http://dx.doi.org/10.1127/ejm/3/2/0231.

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29

Benabdellah, Benabdellah, Karl-Friedrich Albrecht, Valeri L. Pomaz, Elizabeth A. Denisenko, and Dmitrii O. Logofet. "Markov chain models for forest successions in the Erzgebirge, Germany." Ecological Modelling 159, no. 2-3 (January 2003): 145–60. http://dx.doi.org/10.1016/s0304-3800(02)00285-5.

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30

Steinberg, Christian, and Annett Krüger. "Hochmoore im Erzgebirge: Liegt die Störung wirklich in den Mooren?" Wasser und Abfall 13, no. 5 (May 2011): 41–45. http://dx.doi.org/10.1365/s35152-011-0051-y.

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31

Reißmann, Reinhard. "Historical and active mining in the Erzgebirge: Altenberg, Marienberg, Lengefeld." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 97 (March 11, 2015): 185–202. http://dx.doi.org/10.1127/jmogv/97/0009.

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32

Schmitt, U., E. Bäucker, and L. Lehmann. "Zur Morphologie von Nadeln geschädigter Fichten aus dem Ost-Erzgebirge." Forstwissenschaftliches Centralblatt 116, no. 1-6 (December 1997): 381–93. http://dx.doi.org/10.1007/bf02766913.

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33

Weber, Matthias, Manfred Niecke, Kai Gedeon, and Hartmut Meyer. "Quecksilber in Federn des Sperbers (Accipiter nisus) aus dem Erzgebirge." Journal für Ornithologie 142, no. 3 (July 2001): 313–20. http://dx.doi.org/10.1046/j.1439-0361.2001.01006.x.

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34

Weber, Matthias, Manfred Niecke, Kai Gedeon, and Hartmut Meyer. "Quecksilber in Federn des Sperbers(Accipiter nisus) aus dem Erzgebirge." Journal of Ornithology 142, no. 3 (July 2001): 313–20. http://dx.doi.org/10.1007/bf01651370.

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35

Dobrzhinetskaya, Larissa F., Zhenxian Liu, Pierre Cartigny, Junfeng Zhang, Dalila Tchkhetia, Russell J. Hemley, and Harry W. Green. "Synchrotron infrared and Raman spectroscopy of microdiamonds from Erzgebirge, Germany." Earth and Planetary Science Letters 248, no. 1-2 (August 2006): 340–49. http://dx.doi.org/10.1016/j.epsl.2006.05.037.

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36

Walter, Harald, and Hans-Jürgen Berger. "Paleozoic microfossils from the northern margin of the Erzgebirge-Mountains (Saxony)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 209, no. 1 (June 18, 1998): 1–32. http://dx.doi.org/10.1127/njgpa/209/1998/1.

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37

Nasdala, Lutz, and Hans-Joachim Massonne. "Microdiamonds from the Saxonian Erzgebirge, Germany: in situ micro-Raman characterisation." European Journal of Mineralogy 12, no. 2 (March 29, 2000): 495–98. http://dx.doi.org/10.1127/0935-1221/2000/0012-0495.

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38

Schulmann, Karel, Bedřich Mlčoch, and Radek Melka. "High-temperature microstructures and rheology of deformed granite, Erzgebirge, Bohemian Massif." Journal of Structural Geology 18, no. 6 (June 1996): 719–33. http://dx.doi.org/10.1016/s0191-8141(96)80007-1.

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39

Beyrich, F., H. Gräfe, W. Küchler, C. Lindemann, and E. Schaller. "An observational study of sulphur dioxide transport across the Erzgebirge Mountains." Atmospheric Environment 32, no. 6 (March 1998): 1027–38. http://dx.doi.org/10.1016/s1352-2310(97)00363-4.

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40

Barsukov, Vikt L., N. T. Sokolova, and O. M. Ivanitskii. "Metals, arsenic, and sulfur in the Aue and Eibenstock granites, Erzgebirge." Geochemistry International 44, no. 9 (September 2006): 896–911. http://dx.doi.org/10.1134/s0016702906090059.

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41

Velichkin, V. I., and B. P. Vlasov. "Domal structures and hydrothermal uranium deposits of the Erzgebirge, Saxony, Germany." Geology of Ore Deposits 53, no. 1 (February 2011): 74–83. http://dx.doi.org/10.1134/s1075701511010053.

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42

Förster, H. J. "Evolution of the Hercynian Granite Magmatism in the Erzgebirge Metallogenic Province." Mineralogical Magazine 58A, no. 1 (1994): 284–85. http://dx.doi.org/10.1180/minmag.1994.58a.1.149.

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43

Port, A. I. "Book Review: Urangeheimnisse: Das Erzgebirge im Brennpunkt der Weltpolitik 1933-1960." German History 23, no. 2 (April 1, 2005): 287–89. http://dx.doi.org/10.1177/026635540502300224.

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44

Möhn, R. "Medizinische Betrachtungen am Cranach-Altar der St. Wolfgangskirche zu Schneeberg/Erzgebirge." Der Hautarzt 53, no. 9 (September 2002): 622–24. http://dx.doi.org/10.1007/s00105-002-0377-1.

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45

Massonne, Hans-Joachim, and Anita Czambor. "Geochemical signatures of Variscan eclogites from the Saxonian Erzgebirge, central Europe." Geochemistry 67, no. 1 (May 2007): 69–83. http://dx.doi.org/10.1016/j.chemer.2006.07.001.

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46

Keller, Gert. "Radiological aspects of former mining activities in the Saxon Erzgebirge, Germany." Environment International 19, no. 5 (January 1993): 449–54. http://dx.doi.org/10.1016/0160-4120(93)90270-r.

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47

Romer, Rolf L., Rainer Thomas, Holly J. Stein, and Dieter Rhede. "Dating multiply overprinted Sn-mineralized granites—examples from the Erzgebirge, Germany." Mineralium Deposita 42, no. 4 (December 14, 2006): 337–59. http://dx.doi.org/10.1007/s00126-006-0114-2.

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48

Wolkersdorfer, Christian. "Hydrogeochemical investigations of an abandoned uranium mine in the Erzgebirge/Germany." Applied Geochemistry 11, no. 1-2 (January 1996): 237–41. http://dx.doi.org/10.1016/0883-2927(95)00060-7.

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49

Grunewald, Karsten, J. Scheithauer, A. Heiser, Ralf Sudbrack, K. Freier, and H. Andreae. "Einzugsgebiete mit gestörten Hochmooren und ihre Relevanz für Trinkwassertalsperren im Erzgebirge." Wasser und Abfall 11, no. 11 (November 2009): 49–54. http://dx.doi.org/10.1007/bf03247630.

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50

Lorenz, Winfried. "Protolith analysis of metamorphic siliciclastic rocks in the Erzgebirge Mts., Germany." Sedimentary Geology 97, no. 1-2 (June 1995): 43–67. http://dx.doi.org/10.1016/0037-0738(94)00140-p.

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