Search results for "Rust"

A crustal seismic profile across Sicily

2011

Abstract A crustal reflection seismic profile, more than 100 km long, was recorded across central Sicily, from the Tyrrhenian shore to the Sicily Channel, to understand the deep structures and the collision mechanisms between Europe and Africa and the subsequent geodynamic evolution. The profile was acquired using explosive sources and 240 active channels recorded by a Sercel 408-XL, 24 bits A/D converter, with a 12 km spread and a 24-fold coverage. The data were processed following a non-conventional procedure in order to preserve the relative amplitudes of the reflections and to better investigate the Sicily deep structures down to the Moho. The main highlighted structures are the dramati…

The Sicilian collisional boundary. An unconventional carbonate foreland and fold and thrust belt.

2014

Active tectonics, sedimentation history and geomorphological features in the northern Sicily continental margin: implications for the marine geohazar…

2020

Starting from the assumption that seismic events in the active margins are accompanied by evidence of a depositional, geomorphologic and structural type, which constitutes the geological record of their activity, we analysed different features of the Northern Sicily continental margin (NSCM) to reconstruct the deformational field and related stress field in the Southern Tyrrhenian sea. As an outcome of this project we were going to obtain seismotectonic setting and mapping to provide a powerful tool in managing and assessing the marine geological hazards. The study area extends from the San Vito Peninsula to the Termini Gulf along the NSCM, including the Ustica island, and is located in a t…

Solution-mass-transfer deformation adjacent to the Glarus Thrust, with implications for the tectonic evolution of the Alpine wedge in eastern Switzer…

2001

Abstract We have studied aspects of absolute finite strain of sandstones and the deformation history above and below the Glarus Thrust in eastern Switzerland. The dominant deformation mechanism is solution mass transfer (SMT), which resulted in the formation of a semi-penetrative cleavage. Our analysis indicates that the Verrucano and Melser sandstones, which lie above the thrust, were deformed coaxially, with pronounced contraction in a subvertical Z direction and minor extension in a subhorizontal X direction, trending at ∼200°. Most of the contraction in Z was balanced by mass-loss volume strains, averaging ∼36%. Below the Glarus Thrust, sandstones of the North Helvetic flysch have small…

"Table 55" of "Studies of QCD at e+ e- centre-of-mass energies between 91-GeV and 209-GeV."

2004

1-THRUST distribution at c.m. energy 133.00 GeV.

"Table 59" of "Studies of QCD at e+ e- centre-of-mass energies between 91-GeV and 209-GeV."

2004

1-THRUST distribution at c.m. energy 189.00 GeV.

"Table 61" of "Studies of QCD at e+ e- centre-of-mass energies between 91-GeV and 209-GeV."

2004

1-THRUST distribution at c.m. energy 206.00 GeV.

"Table 54" of "Studies of QCD at e+ e- centre-of-mass energies between 91-GeV and 209-GeV."

2004

THRUST distribution at c.m. energy 91.20 GeV.

"Table 56" of "Studies of QCD at e+ e- centre-of-mass energies between 91-GeV and 209-GeV."

2004

1-THRUST distribution at c.m. energy 161.00 GeV.

"Table 57" of "Studies of QCD at e+ e- centre-of-mass energies between 91-GeV and 209-GeV."

2004

1-THRUST distribution at c.m. energy 172.00 GeV.