Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Federico Giovanoli"'
Autor:
Mélissa Ruiz, Urs Schaltegger, Sean P. Gaynor, Massimo Chiaradia, Jürgen Abrecht, Christian Gisler, Federico Giovanoli, Michael Wiederkehr
Publikováno v:
Swiss Journal of Geosciences, Vol 115, Iss 1, Pp 1-24 (2022)
Abstract The Variscan orogeny was responsible for the formation of a significant volume of igneous basement throughout present-day Europe. Detailed understanding of these rocks has, however, been obfuscated by significant overprinting during younger
Externí odkaz:
https://doaj.org/article/1a2d983a4d454680908708c44d9e3327
Publikováno v:
Swiss Journal of Geosciences, Vol 115, Iss 1, Pp 1-23 (2022)
Abstract Drilling of the Gotthard Rail Base Tunnel through the Central Alps from 2005 to 2010 opened up fractured basement units and frequent water inflows provided access to the major fluid-rock interactions processes in orogenic crystalline upper c
Externí odkaz:
https://doaj.org/article/5f2a87ed9d5343928aef104a7355826e
Publikováno v:
Aquatic Sciences. 57:291-304
Sediments in Lake Constance have been dated by radiometric methods and lamination counting. Investigations into the concentrations of lead and zinc in the sediments were carried out to get detailed information about environmental history. Maximum con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::141be9e40f0558a98b30f814f8d2be9c
https://doi.org/10.1007/bf00878394
https://doi.org/10.1007/bf00878394
Autor:
Federico Giovanoli
Publikováno v:
Large Lakes ISBN: 9783642840791
Turbidity currents and interflows are the main mechanisms of transport of suspended particles from rivers to lakes. Turbidity currents originate from singular events—for example, a delta deposit destabilized by unusually high flood waters and its s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53209e3df3b884a2ee83a5c83e1626b5
https://doi.org/10.1007/978-3-642-84077-7_9
https://doi.org/10.1007/978-3-642-84077-7_9
Autor:
Federico Giovanoli, Kenneth J. Hsü
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 29:75-93
Three holes were drilled during the 1975 DSDP Leg 42B drilling the Black Sea. A section from Hole 380, at 2107 m water depth on the western edge of the abyssal plain, is 1074 m thick, and provides the most complete stratigraphic section. Dating of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3d28a4219feff242ebc0b8736b5e5ecc
https://doi.org/10.1016/0031-0182(79)90075-0
https://doi.org/10.1016/0031-0182(79)90075-0