Zobrazeno 1 - 10
of 149
pro vyhledávání: '"William Cavazza"'
Autor:
Ogilvie, Brian W.
Publikováno v:
Isis, 2006 Dec . 97(4), 738-739.
Externí odkaz:
https://www.jstor.org/stable/10.1086/512872
Autor:
Brian W. Ogilvie
Publikováno v:
Isis. 97:738-739
Publikováno v:
Geological Society, London, Special Publications. 520:311-325
Volcanic particles have particular geodynamic significance. Despite abundant datasets on volcanic-derived sand(stone), the distinction between spatial and temporal distribution of volcanic particles within the sedimentary record is poorly documented.
Publikováno v:
Geological Society, London, Special Publications. 523:399-426
Palaeostraits are common features formed during the extension and fragmentation of active continental margins, when back-arc basins are formed and microplates develop through upper-plate extension. In this contribution, we focus on narrow seaways and
Autor:
Thomas Gusmeo, William Cavazza, Massimiliano Zattin, Sveva Corrado, Andrea Schito, Victor Alania, Onise Enukidze
The integration of low-temperature thermochronological and thermal maturity analyses constrains the maximum temperatures experienced during burial by the sedimentary fill of the central sector of the Greater Caucasus basin and the timing of its struc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3489fe65c79fbf0a7f6c6d35421c8b6b
https://doi.org/10.5194/egusphere-egu22-110
https://doi.org/10.5194/egusphere-egu22-110
The Alpine orogenic edifice of Corsica (northern Tyrrhenian Sea) offers the possibility to investigate the mode through which continental crust responds to the propagation of regional shortening at convergent plate margins. The geology of Corsica has
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f85694f4a7b02f83dfd93b3760a4e2b3
https://hdl.handle.net/11590/427853
https://hdl.handle.net/11590/427853
Publikováno v:
Episodes. 42:355-358
Autor:
Victor Alania, William Cavazza, Sveva Corrado, Thomas Gusmeo, Massimiliano Zattin, Onise Enukidze
The 350 km-long Adjara-Trialeti fold-and-thrust belt of southwestern Georgia is the result of the structural inversion of a continental back-arc basin developed in the Paleogene on the upper (Eurasian) plate of the northward subducting northern branc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ab782710eacbffebbc914986d2554e2b
http://hdl.handle.net/11585/797760
http://hdl.handle.net/11585/797760