@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} } @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} } @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} } @inproceedings{SchuesslerOkruschSeideletal.1990, author = {Sch{\"u}ssler, Ulrich and Okrusch, Martin and Seidel, Eberhard and Kreuzer, Hans and Raschka, Helmut}, title = {Pre- to early Variscan magmatism in the Bohemian Massif}, url = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-39171}, year = {1990}, abstract = {No abstract available}, 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{SeidelKreuzerSchuessleretal.1988, author = {Seidel, E. and Kreuzer, H. and Sch{\"u}ssler, Ulrich and Okrusch, M. and Lenz, K.-L. and Raschka, H.}, title = {K-Ar geochronology of the East-Bavarian basement}, url = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-38874}, year = {1988}, abstract = {No abstract available}, language = {en} } @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{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} }