Zobrazeno 1 - 10
of 81
pro vyhledávání: '"Fontignie, D."'
Publikováno v:
Paleoceanography, vol. 23, pp. 1-20
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1900::0e05742ed1003427ea57e1f005163fdf
https://serval.unil.ch/notice/serval:BIB_F5008A13A543
https://serval.unil.ch/notice/serval:BIB_F5008A13A543
Publikováno v:
17th V. M. Goldschmidt Conference in Cologne, Germany, pp. A500
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1900::be13c13c2c2d8fd4a80ee8e5a240bd1c
https://serval.unil.ch/notice/serval:BIB_6ADFF7F6CF75
https://serval.unil.ch/notice/serval:BIB_6ADFF7F6CF75
Autor:
Marzoli A., Bertrand H., Knight K., Nomade S., Verati C., Youbi N., Fontignie D., Bellieni G., Rapaille C.
Publikováno v:
32nd International Geological Congress., Firenze., 2004
info:cnr-pdr/source/autori:Marzoli A., Bertrand H., Knight K., Nomade S., Verati C., Youbi N., Fontignie D., Bellieni G., Rapaille C./congresso_nome:32nd International Geological Congress./congresso_luogo:Firenze./congresso_data:2004/anno:2004/pagina_da:/pagina_a:/intervallo_pagine
info:cnr-pdr/source/autori:Marzoli A., Bertrand H., Knight K., Nomade S., Verati C., Youbi N., Fontignie D., Bellieni G., Rapaille C./congresso_nome:32nd International Geological Congress./congresso_luogo:Firenze./congresso_data:2004/anno:2004/pagina_da:/pagina_a:/intervallo_pagine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::2c35bbe7c6f5c4b150180d0fc9a7d162
https://publications.cnr.it/doc/111912
https://publications.cnr.it/doc/111912
Publikováno v:
Schweizerische Mineralogische und Petrographische Mitteilungen, 84 . pp. 101-117.
Scopus-Elsevier
Schweizerische mineralogische und petrographische Mitteilungen, Vol. 84 (2004) pp. 101-117
Scopus-Elsevier
Schweizerische mineralogische und petrographische Mitteilungen, Vol. 84 (2004) pp. 101-117
The Chelopech volcanic complex is located in the Central Srednogorie magmatic zone and hosts one of the largest Cu–Au deposits in Europe. Field observations and sedimentary relationships allow to distinguish three units of the volcanic complex: (I)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::d02be59d20e0b69eff4d7610dc3f7e78
http://oceanrep.geomar.de/3730/
http://oceanrep.geomar.de/3730/
Young volcanics erupted since late Pliocene as a result of lithospheric extension within the transtensional zones along the NE-SW trending letf-lateral Yumurtalik fault zone that mark the boundary between the African and the Anatolian plates in south
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______9491::d30b86892e2c8ee586837adda7b93a56
https://hdl.handle.net/20.500.12605/22182
https://hdl.handle.net/20.500.12605/22182