ITA  |  ENG

T74. Active faults and crustal deformation in the Mediterranean area from prehistorical to present times: state of the art

-

Congressi SGI-SIMP

Recent years provided significant advancements in understanding active faults and crustal deformation in the Mediterranean area, which includes diverse seismotectonic settings. This was favoured by improvements in methods and technologies applied to paleoseismology, tectonic geomorphology, onshore and offshore geophysical imaging of active faults, tectonic geodesy, geochronology, etc., and by recent earthquakes that provided novel insights on rupture processes, surface deformation patterns and on the deep structures of active faults. However, many seismogenic sources of historical earthquakes remain unidentified and quantitative parameters for several active deformation belts are lacking.
This session aims to foster a discussion on the state-of-the-art of the knowledge on active faults, seismogenic sources and seismotectonic models in the Mediterranean area.
We welcome contributions that provide new insights on:
  1. the investigation of active faults and of their seismogenic potential;
  2. the earthquake sources and of their relationships with known or unknown crustal faults;
  3. the analysis of historical earthquakes and their possible attribution to specific seismogenic sources;
  4. the seismotectonic context and the pattern of strain accumulation and release;
  5. the reconstruction of paleoseismic events through multidisciplinary approaches;
  6. the development of methods for exploring earthquake recurrence.
 
CONVENERS: Luigi Ferranti (Università di Napoli), Francesco Iezzi (Università di Napoli), Andrea Brogi (Università di Bari Aldo Moro), Pierfrancesco Burrato (INGV Roma), Carmelo Monaco (Università di Catania), Fabrizio Pepe (Università di Palermo)

lferrant@unina.it
 
Ultimo aggiornamento:

Articoli correlati

Congressi SGI-SIMP

Active margins, which allow the deciphering of many long-lasting geological processes, probably represent the most complex type of plate boundaries. They inspire ...

Congressi SGI-SIMP

Reservoir and seal rock mechanics are having an increasing importance in georesources studies. Geothermal reservoirs characterization requires different information with ...

Congressi SGI-SIMP

Earthquake mechanics is controlled by processes active over a wide range of scales, from kilometres to nanometres and from seconds to thousands of years. The 3-D ...

Congressi SGI-SIMP

Geological structures capable of generating significant earthquakes release elastic stress accumulated during the interseismic phases at depths of 10-15 km into the ...

Congressi SGI-SIMP

Sedimentary rocks cover most of the Earth's surface and are deposited in different tectonic-geodynamic settings and depositional environments. The combined study of ...

Congressi SGI-SIMP

Accounting for uncertainty in geological models constitutes a crucial challenge for geoscientists, with significant implications for sectors such as exploration, natural ...

Congressi SGI-SIMP

In the past decades, integrated geological and geophysical studies of the subsurface stratigraphic and structural setting of the upper and lower crust have highlighted ...

Congressi SGI-SIMP

The architecture of the Variscan crust and the distribution of its ore deposits is the result of a complex geodynamic history, starting in the early Cambrian with the ...