Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Julien Thomas Fiore"'
Autor:
Atef Onaisi, Federico Selva, Adrian Rodriguez-Herrera, Nick Koutsabeloulis, Julien Thomas Fiore
Publikováno v:
SEG Technical Program Expanded Abstracts 2015.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5dbf46ec1167dc3860234902f98879ac
https://doi.org/10.1190/segam2015-5900945.1
https://doi.org/10.1190/segam2015-5900945.1
Autor:
Anne-Marie Rachoud-Schneider, Julien Thomas Fiore, Walter Wildi, Stéphanie Girardclos, Ira Baster
Publikováno v:
Boreas, Vol. 34, No 4 (2005) pp. 417-433
During the past decade, the presentation of seismic and sedimentological data has allowed reconstruction of the environment and climate history of the Petit-Lac (western Lake Geneva). Methods such as high-resolution seismics, sediment core analysis (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d50107a918f7ed1a7dafe86413a5959
https://doi.org/10.1080/03009480500231385
https://doi.org/10.1080/03009480500231385
Publikováno v:
Géographie physique et Quaternaire. 56:19-32
During the Würmian glaciation, the Jura ice sheet covered the Joux Valley (Vaud, Switzerland). A geomorphological study reveals many drumlins in this valley. Some are composed of gravels and sand, others of till. Outcrops show that the surface of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::80f450d84c8db646133751d73a201d47
https://doi.org/10.7202/008602ar
https://doi.org/10.7202/008602ar
Publikováno v:
Proceedings.
Conventionally, the 4D warping is only performed over the reservoir interval, assuming that all 4D effects are located in the reservoir. In the case of a compacting reservoir, the overburden is affected by subsidence, hence by time shifts. For this p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b07a505f51015e88bd962b4dd83cb9f7
https://doi.org/10.3997/2214-4609.20140763
https://doi.org/10.3997/2214-4609.20140763
Publikováno v:
Quaternary Science Reviews, Vol. 85 (2014) pp. 1-19
Quaternary Science Reviews
Quaternary Science Reviews
Lake Neuchâtel, located at the foothills of the Jura Mountains in Western Switzerland, is one of the numerous perialpine lakes on the Swiss Plateau. It overlies a SW–NE trending paleovalley eroded during Quaternary glaciations through a branch of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8ea50042aee3aaa1a365ee161ca78742
https://archive-ouverte.unige.ch/unige:35976
https://archive-ouverte.unige.ch/unige:35976
Publikováno v:
Quaternary Science Reviews, Vol. 30, No 3-4 (2011) pp. 377-393
Western Lake Geneva (le Petit-Lac) was filled during the Quaternary over a major erosion surface truncating the cemented, folded and thrusted Tertiary sediments of the foreland Alpine basin. The carving of the lake occurred during Quaternary glaciati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3bb1c3a5d9d91d08a7ed6f7b444e08c9
https://archive-ouverte.unige.ch/unige:17243
https://archive-ouverte.unige.ch/unige:17243