Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Thomas Gusmeo"'
Understanding how the brittle deformation pattern at the surface relates to active seismogenic sources at depth is one key element for accurate Seismic Hazard Assessment procedures based on deterministic inputs. Establishing a relationship between su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52ce202a902dcc8336ca5909bda66941
https://doi.org/10.5194/egusphere-egu23-5012
https://doi.org/10.5194/egusphere-egu23-5012
Autor:
Victor Alania, Tamar Beridze, Onise Enukidze, Thomas Gusmeo, Demur Merkviladze, Tamar Shikhashvili, Niko Tevzadze
The Lesser Caucasus (LC) double-wedge orogen accommodates the crustal shortening due to far-field effects of the collision between the Arabian and Eurasian plates. Subsequent convergence of Arabia and Eurasian plates during the late Alpine time cau
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae9e8e221db4b0857e00130430415ddf
https://doi.org/10.5194/egusphere-egu23-2420
https://doi.org/10.5194/egusphere-egu23-2420
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
Autor:
Thomas Gusmeo, William Cavazza, Victor Alania, Onise Enukidze, Massimiliano Zattin, Sveva Corrado, Andrea Schito
Young back-arc rift basins, because of the not yet dissipated extensional thermal signature, are prone to positive inversion following changes in the local geodynamic regime and/or far-Xeld stress transmission. Structural inversion of such basins ten
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::77fa2436872ca567437f349b12017da4
http://hdl.handle.net/11585/885489
http://hdl.handle.net/11585/885489
Autor:
Victor Alania, Massimiliano Zattin, Sveva Corrado, Onise Enukidze, Thomas Gusmeo, William Cavazza
Young back-arc rift basins, because of the not yet dissipated extensional thermal signature, can be easily inverted following changes in the geodynamic regime and/or far-field stress transmission. Structural inversion of such basins mainly develops t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c7872403f8afebb5ef0454909b6a50c
https://doi.org/10.5194/egusphere-egu21-179
https://doi.org/10.5194/egusphere-egu21-179
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
Autor:
Sveva Corrado, Thomas Gusmeo, William Cavazza, Onise Enukidze, Enrico Conventi, Andrea Schito, Victor Alania
Publikováno v:
Marine and Petroleum Geology. 130:105141
Thermal history reconstructions can help to better characterise the geological history of areas that experienced a polyphase tectonic evolution. The integration of published stratigraphic/structural data with new and pre-existing data on thermal matu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::855f50bafc7acbb7a0fd1349fc73e2fe
https://doi.org/10.1016/j.marpetgeo.2021.105141
https://doi.org/10.1016/j.marpetgeo.2021.105141
The Riffelberg-Garten Unit (RGU) is a tectono-stratigraphic unit, belonging to the Zermatt-Saas Zone (ZSZ), characterized by a chaotic mixture of metasediments, metabasites and serpentinites (Bearth, 1967; Dal Piaz & Ernst, 1978; Campari et al., 2004
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::4d7b254bc316644da6886382646c63b7
http://hdl.handle.net/11585/678344
http://hdl.handle.net/11585/678344
Publikováno v:
Scopus-Elsevier
This paper presents a new structural model for the frontal part of the eastern Achara-Trialeti fold- and-thrust belt based on the interpretation of a seismic reflection profile across the retro-wedge of the Lesser Caucasus orogen. The structural deta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::bf9cf430bc5f46858fd8f023983f67fd
http://www.scopus.com/inward/record.url?eid=2-s2.0-85128991339&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-85128991339&partnerID=MN8TOARS