@inproceedings{SchuesslerOkruschRichter1987,
  author    = {Sch{\"u}ssler, Ulrich and Okrusch, M. and Richter, P.},
  title     = {Amphibolites of the KTB target area Oberpfalz, Bavaria},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-38866},
  year      = {1987},
  abstract  = {No abstract available},
  language  = {en}
}
@inproceedings{KreuzerHenjesKunstSeideletal.1993,
  author    = {Kreuzer, H. and Henjes-Kunst, F. and Seidel, E. and Sch{\"u}ssler, Ulrich and B{\"u}hn, B.},
  title     = {Ar-Ar spectra on minerals from KTB and related medium-pressure units},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-86731},
  year      = {1993},
  abstract  = {No abstract available.},
  subject      = {Kontinentales Tiefbohrprogramm},
  language  = {en}
}
@article{ErtlGiesterSchuessleretal.2013,
  author    = {Ertl, Andreas and Giester, Gerald and Sch{\"u}ssler, Ulrich and Br{\"a}tz, Helene and Okrusch, Martin and Tillmanns, Ekkehart and Bank, Hermann},
  title     = {Cu- and Mn-bearing tourmalines from Brazil and Mozambique: crystal structures, chemistry and correlations},
  series = {Mineralogy and Petrology},
  volume    = {107},
  journal   = {Mineralogy and Petrology},
  number    = {2},
  doi       = {10.1007/s00710-012-0234-6},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-127296},
  pages     = {265-279},
  year      = {2013},
  abstract  = {Cu- and Mn-bearing tourmalines from Brazil and Mozambique were characterised chemically (EMPA and LA-ICP-MS) and by X-ray single-crystal structure refinement. All these samples are rich in Al, Li and F (fluor-elbaite) and contain significant amounts of CuO (up to ~1.8 wt\%) and MnO (up to ~3.5 wt\%). Structurally investigated samples show a pronounced positive correlation between the <Y-O> distances and the (Li + Mn\(^{2+}\) + Cu + Fe\(^{2+}\)) content (apfu) at this site with R\(^2\) = 0.90. An excellent negative correlation exists between the <Y-O> distances and the Al\(_2\)O\(_3\) content (R\(^2\) = 0.94). The samples at each locality generally show a strong negative correlation between the X-site vacancies and the (MnO + FeO) content. The Mn content in these tourmalines depends on the availability of Mn, on the formation temperature, as well as on stereochemical constraints. Because of a very weak correlation between MnO and CuO we believe that the Cu content in tourmaline is essentially dependent on the availability of Cu and on stereochemical constraints.},
  language  = {en}
}
@incollection{SchuesslerOkruschSeideletal.1989,
  author    = {Sch{\"u}ssler, Ulrich and Okrusch, M. and Seidel, E. and Richter, P.},
  title     = {Geochemical characteristics of metabasites in different tectonic units of the North-East-Bavarian crystalline basement},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-39221},
  publisher      = {Universit{\"a}t W{\"u}rzburg},
  year      = {1989},
  abstract  = {Comprehensive geochemical investigations of rnetabasites yielded constraints for a correlation of, or discrimination between the different tectonic units within the northeast Bavarian crystalline basement. The M{\"u}nchberg nappe pile consists of at least five large tectonic units which exhibit differences in lithology, in part also in metamorphie grade and in metamorphie history. The metabasites in each of these nappes show their own, significant geochemical characteristics. The lowermost tectonic unit, the Bavarian lithofacies, includes the anchimetamorphie Ordovician Randschieferserie which contains alkaline basalts. In their geochemistry, they are sirnilar to the metabasites of the Fichtelgebirge crystalline complex in the autochthonous Saxo-thuringian. The next higher tectonic unit of the M{\"u}nchberg nappe pile, the Prasinit-Phyllit-Serie contains metabasites which can be derived from subalkaline basalts with a clear calc-alkaline tendency. There is a striking geochemical resemblance to the metabasites of the Erbendorf Greenschist Zone (EGZ) underscorinq the similar lithology of both allochthonous units which appear to be in a similar tectonic position. The Randamphibolit-Serie higher up in the M{\"u}nchberg nappe pile consists of metabasites with tholeiitic characteristics and a pronounced differentiation trend. The next higher tectonic unit, the Liegendserie of the M{\"u}nchberg gneiss cornplex s. str., contains metagabbros to metagabbronorites with a high-Al basaltic composition. The amphibolites and banded hornblende gneisses of the overlying Hangendserie are of subalkaline basaltic character with calc-alkaline affinity. The Zone Erbendorf-Vohenstrauss (ZEV) is currently regarded as an allochthonous unit equivalent to the higher crystalline nappes of the M{\"u}nchberg pile. However, the geochemical character of the metabasites do not encourage such a correlation. Neither the schistose and striped amphibolites nor the flaseramphibolites of the ZEV with their N-KORB and E-MORB character respectively, find convincing counterparts in the crystalline nappes of the M{\"u}nchberg pile. However, an interestingly close resemblance exists between the schistose and striped amphibolites in the ZEV, on the one hand, and in the autochthonous Zone Tirschenreuth- M{\"a}hring (ZTM) and the adjacent Moldanubian sensu strictu, on the other. Owing to the absence of age criteria, our results cannot be used, so far, to reconstruct the paleogeographical position of the individual tectonic units, based on the geochemical characteristics of their respective metabasites.},
  language  = {en}
}
@inproceedings{SchuesslerOkruschRichteretal.1988,
  author    = {Sch{\"u}ssler, Ulrich and Okrusch, M. and Richter, P. and Seidel, E.},
  title     = {Geochemistry of metabasites and element mobility},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-38880},
  year      = {1988},
  abstract  = {No abstract available},
  language  = {en}
}
@inproceedings{SchuesslerVejnarOkruschetal.1988,
  author    = {Sch{\"u}ssler, Ulrich and Vejnar, Z. and Okrusch, M. and Rose, S. and Seidel, E.},
  title     = {Geochemistry of Metabasites and gabbroic rocks from the Tepla-Domazlice zone},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-87511},
  year      = {1988},
  abstract  = {Various amphibolites, metagabbros and eclogitic relics of the Mari{\"a}nske L{\"a}zne complex, and amphibolites from the Cern{\"a} Hora Massif exhibit an uniform geochemical character which compares weil with modern mid-ocean ridge basalts. Geochemically these metabasites are similar to the amphibolites of the Myto area and to schistose, partly striped amphibolites of the neighbouring Tirschenreuth-M{\"a}hring Zone and the Erbendorf-Vohenstrauss Zone (Bavaria). Greenschists and amphibolites from the Domazlice metamorphic complex show an alkaline-basaltic tendency conforming to modern within-plate basalts or basalts from anomalaus midocean ridge segments. In their chemical character, these metabasites compare weil with the flaseramphibolites of the Erbendorf-Vohenstrauss Zone. Fine-grained amphibolites in the Warzenrieth area and (gabbro-) amphibolites in the Bl{\"a}tterberg-Hoher Bogen area show normal MORB character. The metamorphosed gabbroic rocks in the southern part of the Neukirchen-Kdyne (meta-) igneous complex are subalkaline - tholeiitic and exhibit a magmatic differentiation trend. They differ from the neighbouring amphibolites by generally lower contents of incompatible elements.},
  subject      = {Geochemie},
  language  = {en}
}
@article{SchuesslerTalarico1991,
  author    = {Sch{\"u}ssler, Ulrich and Talarico, F.},
  title     = {Granulite facies rocks from the Ross orogenic belt, Northern-Victoria-Land, Antarctica},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-81889},
  year      = {1991},
  abstract  = {no abstract available},
  subject      = {Geographie},
  language  = {en}
}
@inproceedings{KreuzerVejnarSchuessleretal.1988,
  author    = {Kreuzer, Hans and Vejnar, Zdenek and Sch{\"u}ssler, Ulrich and Okrusch, Martin and Seidel, Eberhard},
  title     = {K-Ar dating in the Tepl{\´a}-Domazlice zone at the western margin of the Bohemian Massif},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-31106},
  year      = {1988},
  abstract  = {K-Ar dating on hornblendes and micas from the Tepla Domazlice zone revealed a pattern of dates which significantly deviates from the mid-Carboniferous to early Permian one that is found in the adjacent low-pressure metamorphic Moldanubian and Saxothuringian. Especially for the Marianske Lazne metabasic complex, confirming early Czech determinations, the dates resemble the early Devonian pattern determined for the Munchberg Gneiss Massif and the Erbendorf-Vohenstrau zone of northeastern Bavaria. This supports the idea that all three units are remnants of a huge' complex which suffered a metamorphic overprint under medium-pressure conditions, probably in the early Devonian. Strong rejuvenation is found in the southern part of the Tepla-Domazlice zone by which micas and even two hornblendes were reset to mid-Carboniferous ages. According to the geological setting, part of the apparently preDevonian dates may be explained by inherited argon from earlier metamorphic and magmatic events, e.g. the high-pressure metamorphism documented in eciogitic relics. However, excess argon, caused by the mid-Carboniferous overprint cannot be excluded.},
  language  = {en}
}
@inproceedings{KreuzerVejnarSchuessleretal.1988,
  author    = {Kreuzer, Hans and Vejnar, Zdenek and Sch{\"u}ssler, Ulrich and Okrusch, Martin and Seidel, Eberhard},
  title     = {K-Ar dating of the last metamorphic events in different tectonic units of the western margin of the Bohemian Massif},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-87527},
  year      = {1988},
  abstract  = {K-Ar dating on hornblendes and micas from the Tepl{\"a}Domazlice zone revealed a pattern of dates which significantly deviates from the mid-Carboniferous to early Permian one that is found in the adjacent low-pressure metamorphic Moldanubian and Saxothuringian. Especially for the Mari{\"a}nske L{\"a}zne metabasic complex, confirming early Czech determinations, the dates resemble the early Devonian pattern determined for the M{\"u}nchberg Gneiss Massif and the Erbendorf-Vohenstrauß zone of northeastern Bavaria. This supports the idea that all three units are remnants of a huge complex which suffered a metamorphic overprint under medium-pressure conditions, probably in the early Devonian. Streng rejuvenation is found in the southern part of the Tepl{\"a}-Domailice zone by which micas and even two hornblendes were reset to mid-Carboniferous ages. According to the geological setting, part of the apparently preDevonian dates may be explained by inherited argon from earlier metamorphic and magmatic events, e.g. the high-pressure metamorphism documented in eclogitic relics. However, excess argon, caused by the mid-Carboniferous overprint cannot be excluded.},
  subject      = {Geochemie},
  language  = {en}
}
@article{KreuzerSeidelSchuessleretal.1989,
  author    = {Kreuzer, Hans and Seidel, Eberhard and Sch{\"u}ssler, Ulrich and Okrusch, Martin and Lenz, Karl-Ludwig and Raschka, Helmut},
  title     = {K-Ar geochronology of different tectonic units at the northeastern margin of the Bohemian Massif},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-31811},
  year      = {1989},
  abstract  = {No abstract available},
  language  = {en}
}