Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Paolo Ballato"'
Autor:
Masoud Biralvand, Paolo Ballato, Maria Laura Balestrieri, Mohammad Mohajjel, Edward R. Sobel, Istvan Dunkl, Giordano Montegrossi, Mohammad R. Ghassemi, Johannes Glodny, Manfred R. Strecker
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 1, Pp n/a-n/a (2023)
Abstract The interpretation of low‐temperature thermochronology (LTT) data in magmatic and metallogenic provinces requires a knowledge of the geothermal field through time. There, the challenge is differentiating rapid cooling following transient p
Externí odkaz:
https://doaj.org/article/a7c5aa9b994f4ffaadcb699691016a40
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Externí odkaz:
https://doaj.org/article/8b9cc7ebfce448f98e445361c5e743b3
Autor:
Romano Clementucci, Paolo Ballato, Lionel Siame, Faccenna Claudio, Racano Simone, Torreti Giacomo, Lanari Riccardo, Leanni Laetitia, Valery Guillou
Transient topography represents an opportunity for extracting information on the combined effect of tectonics, mantle-driven processes, lithology and climate across different temporal and spatial scales. The geomorphic signature of transient conditio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8b906a9a92dcde71cc1a58a76381cd54
https://doi.org/10.5194/egusphere-egu23-11243
https://doi.org/10.5194/egusphere-egu23-11243
Autor:
Romano Clementucci, Paolo Ballato, Lionel Siame, Claudio Faccenna, Ahmed Yaaqoub, Abderrahim Essaifi, Laëtitia Leanni, Valery Guillou
Publikováno v:
EGU22
EGU22, 0000, à renseigner, Unknown Region. ⟨10.5194/egusphere-egu22-11675⟩
EGU General Zssembly
EGU General Zssembly, May 2022, Vienna, Austria
EGU22, 0000, à renseigner, Unknown Region. ⟨10.5194/egusphere-egu22-11675⟩
EGU General Zssembly
EGU General Zssembly, May 2022, Vienna, Austria
Topographic relief results from the complex interactions between tectonics and erosional surface processes. The efficiency of surface processes is a function of topographic slopes, bedrock erodibility and climatic conditions. Ancient orogens offers a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::73597fd33864a7f452f79f7dc99a5165
https://hal-insu.archives-ouvertes.fr/insu-03938066
https://hal-insu.archives-ouvertes.fr/insu-03938066
Continental collisional zone may include high-standing plateaus, both internally and externally drained. When endorheic basins are integrated into external drainage networks, the rivers could retain first order information on the capture as well as t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6ae63b094e7693515fba06cd08b63623
https://doi.org/10.5194/icg2022-119
https://doi.org/10.5194/icg2022-119
Autor:
Romano Clementucci, Paolo Ballato, Lionel Louis Siame, Matthew Fox, Riccardo Lanari, Andrea Sembroni, Claudio Faccenna, Ahmed Yaaqoub, Abderrahim Essaifi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5cc92b0cefe6e1999f5e71840dff10ea
https://doi.org/10.1002/essoar.10511350.1
https://doi.org/10.1002/essoar.10511350.1
Autor:
Paolo Ballato, Maria Laura Balestrieri, Istvan Dunkl, Philipp Balling, Mohammad Paknia, Ghasem Heidarzadeh, Masoud Biralvand, Gerold Zeilinger, Mohammad Ghassemi, Claudio Faccenna, Manfred Strecker
The Iranian Plateau represents a NW-SE striking, elongated, elevated (mean elevation of ~1.8 km), arid, mostly internally drained (~65 % of its area) and aseismic morphotectonic feature of the Arabia-Eurasia collision zone. With a crustal thickness u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb5b80d5f0a5c4a50b11d2d84565fd2b
https://doi.org/10.5194/egusphere-egu22-8497
https://doi.org/10.5194/egusphere-egu22-8497
In actively deforming regions, the geometry and evolution of fluvial systems are sensitive to surface uplift, style of deformation and erosion processes. The uplift influences drainages via base level changes, drainage reversals, and capture processe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27ceb2feca0e3e321dd92d170f901b7b
https://doi.org/10.5194/egusphere-egu22-6048
https://doi.org/10.5194/egusphere-egu22-6048
The Central Pontide orogenic belt marks the northern margin of the Central Anatolian Plateau and is the result of several geodynamic processes, including the subduction of the Neo-Tethys crust, the opening of the Black Sea, the continental collision
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ac35408de771fb4e98aba14697fc5be
https://doi.org/10.5194/egusphere-egu22-3939
https://doi.org/10.5194/egusphere-egu22-3939