Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Simona Todaro"'
Publikováno v:
Geosciences, Vol 14, Iss 4, p 89 (2024)
Pressure solution processes taking place during diagenesis deeply modify the hydraulic properties of carbonates, affecting their mechanical layering and hence the dimension, distribution, and connectivity of high-angle fractures. The formation of sty
Externí odkaz:
https://doaj.org/article/86191839836e4d65818bdf8c94482750
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
The Triassic/Jurassic boundary section cropping out at Mt Sparagio in north-western Sicily (Italy) consists of a thick and continuous peritidal succession typical of a Tethyan carbonate platform. The combined chemostratigraphic and biostratigraphic s
Externí odkaz:
https://doaj.org/article/b1957fec6e084fe1bfd22530513cdcc7
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 120, Iss 1 (2014)
New biostratigraphic data, based on conodont investigations, were collected from the Ladinian limestones recently described at Sant’Otiero, a locality near the Village of Petralia Sottana in the Madonie Mountains (Central-Northern Sicily). At this
Externí odkaz:
https://doaj.org/article/37c322b7c3fc4079b74d4d42ef75e7b9
The study carbonates are exposed in the axial zone of the southern Apennines ftb, Italy. These rocks form a natural laboratory to investigate the time-dependent variation of primary heterogeneities and both dimensional properties and distribution of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42aaf6b7f32c43db7e63d8aa7fafc59d
https://doi.org/10.5194/egusphere-egu23-5630
https://doi.org/10.5194/egusphere-egu23-5630
In this study we present the results of a seismic-stratigraphic analysis of sub-bottom profiles in the north-westernmost area of the Malta Plateau in order to define the depositional mechanisms for the upper Quaternary sequences. During this interval
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0c0164cbc160c8cd76473d75e0571281
http://hdl.handle.net/10447/537238
http://hdl.handle.net/10447/537238
The presence of a huge carbonate slope of Cretaceous age is recorded in some imbricated thrust sheets from the Maghrebian fold-and-thrust belt cropping out in northwesternmost Sicily (southern Italy). The sedimentological features of this escarpment,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8f7d63fa13d03bf6ab41e6039942f9a2
http://hdl.handle.net/10447/404006
http://hdl.handle.net/10447/404006
An enormous sulfur isotope excursion indicates marine anoxia during the end-Triassic mass extinction
Autor:
Jacopo Dal Corso, Paul B. Wignall, Tianchen He, Robert J. Newton, Rosemary E. Jones, Robert A. Jamieson, Manuel Rigo, Benjamin J. W. Mills, Emily C. Turner, Simona Todaro, Alexander M. Dunhill, Vincenzo Randazzo, Pietro Di Stefano
The role of ocean anoxia as a cause of the end-Triassic marine mass extinction is widely debated. Here, we present carbonate-associated sulfate δ34S data from sections spanning the Late Triassic–Early Jurassic transition, which document synchronou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b290d881f0f430bf1fcc3ca951eca99e
http://hdl.handle.net/10447/473251
http://hdl.handle.net/10447/473251
Autor:
Daniele Spatola, Attilio Sulli, Aaron Micallef, Gualtiero Basilone, Simona Todaro, P. Di Stefano
A high resolution seismic stratigraphic study of the western edge of the Malta Plateau (central Mediterranean Sea) was conducted to reconstruct the depositional mechanisms of the shelf-slope system since the end of the Messinian salinity crisis (MSC;
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6cc6192b9fd76d952e5d3dd14b20e1aa
http://hdl.handle.net/11573/1645519
http://hdl.handle.net/11573/1645519
Autor:
Fabrizio Pepe, Pietro Renda, Nicolò Parrino, Francesco Cavalcante, Fabrizio Agosta, R. Giarrusso, Emanuele Tondi, P. Di Stefano, Simona Todaro
Publikováno v:
Marine and Petroleum Geology. 135:105400
This study aims at evaluating the control exerted by fracture stratigraphy and diagenetic processes on oil first migration through an outcropping, mixed carbonate-siliciclastic succession. The present work included results of sedimentological, paleon