A5008724323- earthquake and tectonic studies
- Geological and Geochemical Analysis
- Geological and Geophysical Studies Worldwide
- Geological formations and processes
- High-pressure geophysics and materials
- Landslides and related hazards
- Seismic Imaging and Inversion Techniques
- Geology and Paleoclimatology Research
- Geological Modeling and Analysis
- 3D Surveying and Cultural Heritage
- Geological Formations and Processes Exploration
- Hydrocarbon exploration and reservoir analysis
- Rock Mechanics and Modeling
- Paleontology and Stratigraphy of Fossils
- Hydraulic Fracturing and Reservoir Analysis
- Maritime and Coastal Archaeology
- Seismic Waves and Analysis
- Methane Hydrates and Related Phenomena
- Drilling and Well Engineering
- Geophysical Methods and Applications
- Geotourism and Geoheritage Conservation
- Archaeological and Geological Studies
- Geochemistry and Geologic Mapping
- Building materials and conservation
- Geological Studies and Exploration
University of Basilicata
2016-2025
Polo d’Innovazione di Genomica
2023
Istituto Nazionale di Geofisica e Vulcanologia
2023
University of Bari Aldo Moro
2023
University of Naples Federico II
2008
University of Siena
2004-2005
Institute of Refrigeration
1999
University of Padua
1991
The Val d'Agri Basin is a Quaternary sedimentary basin topping multiple tectonic units of the southern Apennines fold-and-thrust belt and giant oilfield within deeper Apulian Platform carbonates. This bounded by seismically active East Agri (EAFS) Monti della Maddalena (MMFS) extensional fault systems. reservoir rocks are sealed separated from shallower thrust sheets clay-rich overpressured mélange. role this mélange during evolution at shallow crustal levels widely debated perhaps...
Understanding the impact of local stress states on computed permeability for fractured carbonates or any other lithotype is crucial to better assess modalities fluid flow in subsurface. Considering Mesozoic exposed along flanks Viggiano Mt. southern Italy, we investigate control exerted by fracture networks output DFN modelling geocellular volumes whose dimensions are like those studied outcrops. Specifically, following four sedimentary units considered:Scarrone La Macchia II, (SLM II),...
Research Article| October 01, 2002 Interplay between tectonics and glacio-eustasy: Pleistocene succession of the Crotone basin, Calabria (southern Italy) F. Massari; Massari 1Dipartimento di Geologia, Paleontologia e Geofisica, Università Padova, Via Giotto 1, 35137 Italy Search for other works by this author on: GSW Google Scholar D. Rio; Rio M. Sgavetti; Sgavetti 2Dipartimento Scienze della Terra, Parma, Viale delle Scienze, 78, 43100 G. Prosser; Prosser 3Dipartimento Geologiche Basilicata...
Abstract The complex development of the northern Crotone Basin, a forearc basin Calabrian Arc (Southern Italy), has been documented by sedimentological, stratigraphic and structural analyses. This Mediterranean‐type fault bounded consists small depocentres commonly characterized mix facies that grades from continental to shallow marine. lower Pliocene infill Basin offshore marls (Cavalieri Marl) grade upwards into shallow‐marine succession up 850 m thick (Zinga Formation). is subdivided...
Abstract The C rotone B asin was generated in the late enozoic as a forearc basin of I onian arc‐trench system. New data are gained through detailed field mapping, high‐resolution stratigraphic analysis key area and examination offshore well seismic reflection profiles. Major unconformities divide fill into major sequences, which reveal three‐stage internal organization thought to reflect geodynamic events alabrian arc backarc closely. first stage is characterized by extensional block...
This paper presents an investigation into technologies of wireless intelligent sensor networks for refrigerated delivery vehicle. The has reviewed the latest communication such as Bluetooth and Zigbee, artificial neural network, fuzzy logic neuro-fuzzy. A proposed solution future cold chain area been addressed.
The proposed geological itinerary connects a series of impressive outcrops distributed between the front and inner portion Southern Apennine thrust belt. It offers opportunity to visit some most interesting best-exposed geosites, inserted within landscapes typical different sectors belt, in order illustrate its evolution. has been designed such way as intersect stacked tectonic units great variety sedimentary successions whose age ranges from Triassic Pleistocene. Each chosen geosite...
This work focuses on the spacing and height distributions of bed-perpendicular fracture sets present within a carbonate multilayer, their effect volumetric (P32 porosity) hydraulic (correspondent permeability) properties rock mass computed after DFN modelling. Results integrated field laboratory analyses are consistent with an uneven distribution Strata-Bound (SB) fractures. The oldest SB fractures formed individual limestone beds bounded by bed interfaces, which likely acted as mechanical...
The Southern Apennines consist of a Cenozoic to Quaternary fold and thrust belt characterized by complex structural architecture. In the axial portion chain, corresponding Agri Valley, folds faults with multiple styles formed during progressive emplacement various tectonic units, derived from different paleodomains. available geological maps, geometry these structures is often hindered scarce cartographic detail due use basic stratigraphic subdivisions. Therefore, at aim better define...