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  • 1989 (2)
  • 1988 (2)

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  • Geochemie (1)
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  • Schüssler, Ulrich (4)
  • Seidel, E. (4)
  • Vejnar, Z. (4)
  • Okrusch, M. (3)
  • Kopecký, L. (1)
  • Kreuzer, H. (1)
  • Kreuzer, H.. (1)
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Geochemistry of metabasites and gabbroic rocks from the Tepla-Domazlice zone. (1988)
Schüssler, Ulrich ; Vejnar, Z. ; Okrusch, Martin ; Rose, D. ; Seidel, E.
Various amphibolites, metagabbros and eclogitic relics of the Mariimske Lazne complex, and amphibolites from the Cerna Hora Massif exhibit an uniform geochemical character which compares well with modern mid-ocean ridge basalts. Geochemically these metabasites are similar to the amphibolites of the My to area and to schistose. partly striped amphibolites of the neighbouring Tirschenreuth-Mahring Zone and the Erbendorf-Vohenstrauss Zone (Bavaria). Greenschists and amphibolites from the Domailice metamorphic complex show an alkaline-basaltic tendency conforming to modern within-plate basalts or basalts from anomalous midocean ridge segments. In their chemical character, these metabasites compare well with the flaseramphibolites of the Erbendorf-Vohenstrauss Zone. Fine-grained amphibolites in the Warzenrieth area and gabbroic amphiboltes in the Blatterberg-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.
Ar-Ar Datierungen am NW-Rand der Böhmischen Masse (1989)
Schüssler, Ulrich ; Kreuzer, H. ; Okrusch, M. ; Raschka, H. ; Seidel, E. ; Vejnar, Z.
No abstract available
Geochemische Untersuchungen und K-Ar Datierungen in der Zone Tepl-Taus (1989)
Schüssler, Ulrich ; Kreuzer, H.. ; Vejnar, Z. ; Okrusch, M. ; Seidel, E. ; Kopecký, L. ; Patzak, M.
no abstract available
Geochemistry of Metabasites and gabbroic rocks from the Tepla-Domazlice zone (1988)
Schüssler, Ulrich ; Vejnar, Z. ; Okrusch, M. ; Rose, S. ; Seidel, E.
Various amphibolites, metagabbros and eclogitic relics of the Mariänske Läzne complex, and amphibolites from the Cernä 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-Mähring 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 Blätterberg-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.
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