Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Franz Vavtar"'
Autor:
Thomas Koch Waldner, Susanne Klemm, Gerald Hiebel, Caroline Grutsch, Klaus Hanke, Markus Staudt, Bernard Moulin, Eric Thirault, Joël Vital, Rudolf Klopfer, Astrid Stobbe, Rüdiger Krause, Klaus-Peter Martinek, Peter Tropper, Joachim Lutz, Manuel Scherer-Windisch, Kurt Nicolussi, Thomas Pichler, Matthias Krismer, Daniel Bechter, Martin Steiner, Hans-Peter Viertler, Franz Vavtar, Simon Timberlake, Leandra Reitmaier-Naef, Monika Oberhänsli, Mathias Seifert, Niels Bleicher, Werner H. Schoch, Thomas Reitmaier, Philippe Della Casa, Elena Silvestri, Paolo Bellintani, Andreas Hauptmann, Roman Lamprecht, Bianca Zerobin, Ulrike Töchterle, Erica Hanning, Roland Haubner, Susanne Strobl, Peter Trebsche, Sebastian Krutter, Ernst Pernicka, Daniel Modl, Stephan Möslein
Publikováno v:
Der Anschnitt, Beihefte ISBN: 9783867570343
The exploitation of copper deposits in the mountainous areas of the Alps gained enormous economic importance particularly in the 2nd and 1st millennium B.C., as Alpine copper began to play a central role in the metal supply of Europe. This volume sum
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f5f6a585204d810aa7a08f1e27ad7e5
https://doi.org/10.46586/dbm.179
https://doi.org/10.46586/dbm.179
Publikováno v:
Archaeometry. 55:923-945
The prehistoric settlement on the Kiechlberg hilltop is located a few kilometres to the north-east of Innsbruck, in the Tyrolean Inn Valley. Despite its rather isolated location, a multiphase settlement between the fifth and the second millennium bc
Publikováno v:
European Journal of Mineralogy. 23:925-936
The copper ore occurrences from Schwaz and Brixlegg were mined both in prehistoric and historic times. The ores occur as discordant veins, strata-bound bodies and breccias in the Devonian Schwaz Dolomite of the Northern Greywacke Zone. The ore minera
Publikováno v:
Neues Jahrbuch für Mineralogie - Abhandlungen. 187:207-215
Publikováno v:
Ore Geology Reviews. 31:319-336
The Woxi W–Sb–Au deposit in Hunan, South China, is hosted by Proterozoic metasedimentary rocks, a turbiditic sequence of slightly metamorphosed (greenschist facies), gray-green and purplish red graywacke, siltstone, sandy slate, and slate. The mi