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pro vyhledávání: '"Isabella Haas"'
Allanite-group minerals are known to incorporate not only U and Th but also initial, non-radiogenic Pb. Allanite can therefore be analyzed in order to assess its crystallization age as well as the ambient Pb composition at the time of crystallization
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71f9236c535194c97b1ad2b107abbdf3
https://doi.org/10.5194/egusphere-egu23-8976
https://doi.org/10.5194/egusphere-egu23-8976
The Schladming Nappe, as a part of the Silvretta-Seckau Nappe System of the Eastern Alps, comprises pre-Alpine remnants of crystalline basement rocks which give important information for reconstructing the Variscan and even pre-Variscan history of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d7b1c8af2f77287632f809a959a1c12
https://doi.org/10.5194/egusphere-egu22-4246
https://doi.org/10.5194/egusphere-egu22-4246
Autor:
Stefanie Eichinger, Josef Nievoll, Doria Haller, Harald Fritz, Dorothee Hippler, Christoph Hauzenberger, Isabella Haas, Magdalena Mandl
Publikováno v:
Gondwana Research. 77:204-222
We compare detrital U/Pb zircon age spectra of Carboniferous and Permian / Lower Triassic sedimentary rocks from different structural positions within the Austroalpine nappe pile with published ages of magmatic and metamorphic events in the Eastern A
The crystalline basement of the Schladming Nappe, Eastern Alps, is part of the Silvretta-Seckau Nappe system. It consists mainly of ortho- and paragneisses which were intruded by slightly overprinted granites and granodiorites. On top of the basement
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::594cce9b5921d4747bc48603164bfa27
https://doi.org/10.5194/egusphere-egu2020-5654
https://doi.org/10.5194/egusphere-egu2020-5654