Academic literature on the topic 'NE Friuli'

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Journal articles on the topic "NE Friuli"

1

Patricelli, Giulia, Maria Eliana Poli, and Daniele Cheloni. "Structural Complexity and Seismogenesis: The Role of the Transpressive Structures in the 1976 Friuli Earthquakes (Eastern Southern Alps, NE Italy)." Geosciences 12, no. 6 (2022): 227. http://dx.doi.org/10.3390/geosciences12060227.

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We reconstructed the seismotectonic setting of the area comprising the northeastern Friuli Plain and the Julian pre-Alpine border (NE Italy) by integrating geological and seismological data. The study area represents the junction between the SSE-verging polyphase thrust-front of the south-Alpine Chain and the NW–SE-trending strike-slip faults of the eastern Friuli–western Slovenia domain. Following a multidisciplinary approach, the 3D geometry of the Susans–Tricesimo thrust system was reconstructed through the elaboration of four geological cross sections derived from the interpretation of ENI industrial seismic lines. In a second step, the seismogenic volume of the central-eastern Friuli area was investigated through hypocentral distribution analysis: the seismic events of the latest 50 years (1976–1977 and 1978–2019 time intervals) were plotted on four NE-SW-oriented seriated sections together with the fault plane’s geometry. Through this procedure, we were able to investigate the relationship between the NW-SE-striking high-angle faults, which characterize the northern Julian pre-Alps, and the WSW-verging medium-angle reverse fronts located at the piedmont of the Friuli plain, which experienced NW-SE- to NNW-SSE-oriented compression starting at least from the Pliocene. In detail, we examined the involvement of these structures during the seismic sequences of May and September 1976, in terms of activation and/or interaction. The resulting seismotectonic model highlights the interplay between transpressive/strike-slip and reverse planes. In particular, this study suggests that Predjama and Maniaglia transpressive faults strongly control the stress release and likely played a fundamental role both during the 6 May (Mw 6.5) and 15 September (Mw 6.0) Friuli earthquakes.
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2

Calligaris, Chiara, Stefano Devoto, and Luca Zini. "Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)." Journal of Maps 13, no. 2 (2017): 406–14. http://dx.doi.org/10.1080/17445647.2017.1316321.

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3

Bertoldi, Maria L., Angelo Boemo, Fabrizio Martini, and Francesco Sguazzin. "Gagea spathacea(Hayne) Salisb. in the lowland woods of Eastern Friuli (NE Italy)." Webbia 64, no. 1 (2009): 17–22. http://dx.doi.org/10.1080/00837792.2009.10670850.

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4

Aoudia, A., A. Saraó, B. Bukchin, and P. Suhadolc. "The 1976 Friuli (NE Italy) thrust faulting earthquake: A reappraisal 23 years later." Geophysical Research Letters 27, no. 4 (2000): 573–76. http://dx.doi.org/10.1029/1999gl011071.

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5

Cauzzi, Carlo, Ezio Faccioli, and Giovanni Costa. "1D and 2D site amplification effects at Tarcento (Friuli, NE Italy), 30 years later." Journal of Seismology 15, no. 1 (2010): 1–17. http://dx.doi.org/10.1007/s10950-010-9202-y.

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6

Finco, Franco, and Luca Melchior. "‘Toponimi esposti’ in lingua minoritaria nella regione Friuli Venezia Giulia." apropos [Perspektiven auf die Romania], no. 8 (July 26, 2022): 119–52. http://dx.doi.org/10.15460/apropos.8.1924.

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In aree plurilingui, l’esposizione di indicazioni toponimiche in lingue diverse costituisce un contributo fondamentale per garantire la visibilità delle lingue del territorio. Nel caso di comunità linguistiche minoritarie con spiccata frammentazione dialettale, con una varietà di riferimento di recente codificazione o prive di essa, nonché in zone con scarso orientamento verso una norma esogena (isole linguistiche, ma talora anche territori di confine), la decisione di esporre toponimi in più lingue non è tuttavia scevra di problemi: va prediletta la forma locale, spesso di diffusione limitata, o una forma sovralocale? Nel caso di lingue non codificate, a quale tradizione grafica ci si deve orientare? All’esempio del Friuli Venezia Giulia, nel nordest d’Italia, illustreremo come le scelte toponimiche, talora contrastanti a seconda degli attori che le attuano, possano suscitare irritazioni e reazioni negative nella popolazione. Cercheremo poi di indagare i motivi che guidano tali scelte e quale cultura della memoria ne emerga.
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7

Pipan, P., and M. Zorn. "Public participation in recovery after earthquakes in Friuli (NE Italy) and the Upper Soča Valley (NW Slovenia) in 1976, 1998, and 2004." Natural Hazards and Earth System Sciences Discussions 1, no. 3 (2013): 2231–53. http://dx.doi.org/10.5194/nhessd-1-2231-2013.

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Abstract. The article deals with public participation in recovery after earthquakes in the border region of Friuli (NE Italy) and the Upper Soča Valley (NW Slovenia) in 1976 (magnitude 6.4, 6 May; magnitude 6.1, 15 September), 1998 (magnitude 6.0, 12 April), and 2004 (magnitude 4.9, 7 July). It highlights the differences in the concepts of the post-earthquake recovery, taking into consideration the different political systems between the two countries (capitalist Italy vs. communist Slovenia in 1976) and changes in recovery after the change of political system in Slovenia (communist Slovenia in 1976 vs. capitalist Slovenia in 1998 and 2004).
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8

Nardi, Gianluca, and Paolo Audisio. "Italian account for Stephanopachys linearis (Kugelann, 1792), a species listed in Annex II of the Habitats Directive (Coleoptera: Bostrichidae)." Fragmenta Entomologica 48, no. 2 (2016): 131. http://dx.doi.org/10.4081/fe.2016.185.

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Three old specimens of <em>Stephanopachys</em> <em>linearis</em> (Kugelann, 1792) from NE Italy, Udine Province (Friuli-Venezia Giulia Region) are recorded. This is the first certain record of this species for Italy since the only previous records, from South Tyrol, were doubtful. This new record is of high conservation value, since this species is protected by the Habitats Directive in the European Union. Distributional and biological data on <em>S. linearis</em> are summarized and it is documented that the previous, doubtful literature records from South Tyrol are erroneous.
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9

PIERI, Valentina, Koen MARTENS, Fabio STOCH, and Giampaolo ROSSETTI. "Distribution and ecology of non-marine ostracods (Crustacea, Ostracoda) from Friuli Venezia Giulia (NE Italy)." Journal of Limnology 68, no. 1 (2009): 1. http://dx.doi.org/10.4081/jlimnol.2009.1.

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10

Singh, D. D., A. Govoni, and P. L. Bragato. "Coda Q c Attenuation and Source Parameter Analysis in Friuli (NE Italy) and its Vicinity." pure and applied geophysics 158, no. 9 (2001): 1737–61. http://dx.doi.org/10.1007/pl00022508.

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