Zobrazeno 1 - 10
of 96
pro vyhledávání: '"S. Hoernes"'
Publikováno v:
Contributions to Mineralogy and Petrology. 178
Geochemical and isotopic data are presented for ~ 32 Ma-old high-K andesites and dacites from the Alpine Chain. The samples consist of plagioclase, amphibole, titanomagnetite and rare biotite and quartz. Geochemical and isotope data indicate that sla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc60c011ba6447b13656e9f9646227b7
https://doi.org/10.1007/s00410-022-01983-w
https://doi.org/10.1007/s00410-022-01983-w
Akademický článek
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Akademický článek
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Publikováno v:
Mineralogical Magazine. 70:545-564
Deerite, a typical mineral of Fe-rich metacherts metamorphosed under blueschist conditions, is not rare, but known occurrences have up to now been restricted mainly to the Tethyan collisional zone and the Western Cordillera of North America. We descr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::799a124acf9dd99113bc81faba4ad70d
https://doi.org/10.1180/0026461067050349
https://doi.org/10.1180/0026461067050349
Publikováno v:
Mineralogy and Petrology. 49:175-188
Transitions between graphitic gneisses, graphite-bearing calcsilicate rocks and marbles of the Variegated Sequence (Bunte Serie) in the Moldanubian zone of the Bohemian massif were examined for their primary sedimentary signatures. The bulk chemistry
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bd60d514527f1f75ae8f2cf2a29700d1
https://doi.org/10.1007/bf01164593
https://doi.org/10.1007/bf01164593
Publikováno v:
Precambrian Research. 66:1-2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::05392fb8f8910a4752d45d99e78c2b47
https://doi.org/10.1016/0301-9268(94)90040-x
https://doi.org/10.1016/0301-9268(94)90040-x
Autor:
H. Friedrichsen, S. Hoernes
Publikováno v:
Contributions to Mineralogy and Petrology. 67:305-315
123 mineral separates from 37 rock samples of the northern Otztal-Stubai Alps have been analysed for their oxygen- and 38 minerals for their hydrogen isotopic composition. The results confirm that alpine metamorphism had little influence on the rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c2b2a9058af507f5ed78ce453e26abd8
https://doi.org/10.1007/bf00381458
https://doi.org/10.1007/bf00381458
Autor:
S. Hoernes
Publikováno v:
TMPM Tschermaks Mineralogische und Petrographische Mitteilungen. 20:81-106
In einem metamorphen Gebiet (westliche Hohe Tauern, Osterreich), das P-T-Bedingungen von der niedrigen Grunschieferfazies bis zur Amphibolitfazies zeigt, wird die aufsteigende Metamorphose in ehemals pelitischen, mergeligen sowie in basaltischen und
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9bcfc0fd678eb61795e66ecba88d7211
https://doi.org/10.1007/bf01081386
https://doi.org/10.1007/bf01081386
Publikováno v:
Contributions to Mineralogy and Petrology. 35:34-42
Paragonite occurs in pelitic schists and amphibole schists of the Otztal Alps (Tyrol); its occurence in amphibole schists is controlled by the Na2O/K2O, in pelitic schists by the local fabric. Some analysis of the bulk chemistry of the paragonite bea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1427c49351d5ad6ddca195131a9bd845
https://doi.org/10.1007/bf00397375
https://doi.org/10.1007/bf00397375
Autor:
S. Hoernes, H. Friedrichsen
Publikováno v:
Initial Reports of the Deep Sea Drilling Project, 65
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a830fc1d464b99cf1a554092d0d485b7
https://doi.org/10.2973/dsdp.proc.65.132.1983
https://doi.org/10.2973/dsdp.proc.65.132.1983
