1,720,974 research outputs found
Teofilo G. Pons (1895-1991)
No full textGenre Arturo. Teofilo G. Pons (1895-1991). In: Le Monde alpin et rhodanien. Revue régionale d'ethnologie, n°4/1991. pp. 116-118
Pons (Teofilo G.) Vita montanara e folklore nelle valli valdesi
No full textSéguy Jean. Pons (Teofilo G.) Vita montanara e folklore nelle valli valdesi. In: Archives de sciences sociales des religions, n°47/2, 1979. p. 290
Pons (Teofilo G.). — Dizionario del dialetto valdese délia Val Germanasca, collana délia Società di Studi Valdesi, n° 6, Torre Pellice, 1973
No full textTuaillon Gaston. Pons (Teofilo G.). — Dizionario del dialetto valdese délia Val Germanasca, collana délia Società di Studi Valdesi, n° 6, Torre Pellice, 1973. In: Le Monde alpin et rhodanien. Revue régionale d'ethnologie, n°3-4/1973. pp. 167-168
La vie traditionnelle dans les Vallées Vaudoises du Piémont. Traduit et adapté de l'italien par V. Bettega, C. Abry, C. Joisten
No full textPons Teofilo G., Bettega Victor, Abry Christian, Joisten Charles. La vie traditionnelle dans les Vallées Vaudoises du Piémont. Traduit et adapté de l'italien par V. Bettega, C. Abry, C. Joisten. In: Le Monde alpin et rhodanien. Revue régionale d'ethnologie, n°3-4/1978. pp. 7-161
Neogene-Quaternary evolution of the offshore sector of the Southern Apennines accretionary wedge, Gulf of Taranto, Italy
No full textSouthern Apennines represent a collisional orogenic belt whose compressional regime is commonly assumed to have ceased during Middle Quaternary. On the other hand, to the south the Calabria Arc is still characterized by subduction and the principal aim of the present research is to shed some light on the space and time transition from the ceased collision to the active subduction. Accordingly, we investigated the offshore sector of the Southern Apennines accretionary wedge, corresponding to the Taranto Gulf. To gain insights into the offshore accretionary wedge, we reconstructed a 3D geological and tectonic model by interpreting a grid of 40 seismic reflection lines (1100 km, 80 intersections), within an area of ca. 10(4) km(2), calibrated with 17 wells. The geometric and chronological constraints allow documenting a systematic Messinian-Quaternary thrust migration from internal towards external sectors of the wedge. The migrating deformational process was essentially associated with a leading-imbricate thrust system with a general NE-younging direction, where we could recognize and distinguish some major advancing phases characterized by alternating fast thrust propagation events and strain accumulation periods within the wedge. This process is well emphasized by the jump of the foredeep and piggy-back basins. The NE-wards wedge migration was also associated with a lithospheric-scale flexural folding that generated a set of normal faults striking parallel to the coeval thrusts, likely reactivating optimally oriented structures inherited from Mesozoic events. Finally, a persisting thrust activity up to the latest Quaternary and possibly up to Present in correspondence of the extemalmost sector of the accretionary wedge has been documented and explained in terms of strain partitioning in the frame of a recent oblique convergence. The results of this research have possible implications for the seismic hazard assessment of the broader region which is possibly greater than previously assumed
Integrated Geomorphological and Geospatial Analysis for Mapping Fluvial Landforms in Murge Basse Karst of Apulia (Southern Italy)
No full textAn integrated geomorphological and geospatial study was performed in order to map fluvial landforms in a sector of Lama Lamasinata close to the town of Binetto in the Murge Basse karst (metropolitan area of Bari, Apulia, Southern Italy). This study describes a combined approach, based on geomorphological fieldwork and topographical position index (TPI)-based landform classification, aimed at identifying the main landforms in an anthropically-modified environment, which suffered a progressive transformation of original morphologies. The resulting geomorphological map of fluvial features was then compared with the available cartography in order to highlight the main strength of the applied methodology in mapping fluvial landforms. Moreover, semi-automatic landform classification was performed for the entire catchment of the Lama Lamasinata in order to evaluate the usefulness of the approach for the fast and objective delimitation of widespread geomorphological elements of the Murge area such as flat-bottomed valleys with steep- or gently-dipping flanks and relict incised valleys. We demonstrated that such an approach can effciently support land use planning in an area affected by hydrogeological hazards
Going Beyond Counting First Authors in Author Co-citation Analysis
Full text linkThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
Stratigraphic constraints about timing of the Tremiti ridge uplift (offshore Apulia, southern Italy)
No full textSeismic monitoring of underground activities for energy production: Survey of the existing facilities with reference to the Italian monitoring guidelines
No full textThis paper reports the results of a study aimed at analyzing the existing seismic monitoring infrastructures of underground activities for energy production. The study was carried out by the Italian National Institute of Oceanography and Applied Geophysics (OGS), in collaboration with the Italian National Research Council - Institute for Electromagnetic Detection of the Environment (CNRIREA), in the framework of the partnership established by the Ministry of Economic Development, Directorate General for Safety of Mining and Energy Activities - National Mining Office for Hydrocarbons and Georesources (MiSE DGS-UNMIG), with Italian Universities and Research Institutions within the so-called "Network for Offshore Safety". Firstly, a survey was carried out by sending a questionnaire to companies to gather information about the infrastructures and procedures for monitoring seismicity, ground deformation and pore pressure, respectively, implemented within the hydrocarbon exploitation fields for either production or re-injection or gas-storage currently present in Italy. Then, the data obtained by the survey were analyzed with reference to the requirements of the "Italian Guidelines for monitoring the seismicity, underground deformation and pore pressure" (ILG) (Dialuce et al., 2014), in order to establish the possible needs for upgrading and, subsequently, assessing the relative costs. This paper reports the evaluation of the technical part, i.e. that concerning the upgrade of the monitoring systems
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