Relevant bibliographies by topics / Pinacoteca nazionale (Ferrara, Italy)

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Academic literature on the topic 'Pinacoteca nazionale (Ferrara, Italy)'

Author: Grafiati
Published: 26 July 2024
Last updated: 31 July 2025

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Journal articles on the topic "Pinacoteca nazionale (Ferrara, Italy)"

1

Pesaresi, D., M. Romanelli, C. Barnaba, P. L. Bragato, and G. Durì. "OGS improvements in 2012 in running the North-eastern Italy Seismic Network: the Ferrara VBB borehole seismic station." Advances in Geosciences 36 (July 22, 2014): 61–67. http://dx.doi.org/10.5194/adgeo-36-61-2014.

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Abstract. The Centro di Ricerche Sismologiche (CRS, Seismological Research Centre) of the Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS, Italian National Institute for Oceanography and Experimental Geophysics) in Udine (Italy) after the strong earthquake of magnitude M=6.4 occurred in 1976 in the Italian Friuli-Venezia Giulia region, started to operate the North-eastern Italy Seismic Network: it currently consists of 17 very sensitive broad band and 18 simpler short period seismic stations, all telemetered to and acquired in real time at the OGS-CRS data centre in Udine.
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2

Delle Foglie, Anna, and Anna Felici. "The Iridescent Painting Palette of Michelino da Besozzo: First Results of Non-Invasive Diagnostic Analyses." Heritage 7, no. 6 (2024): 3013–33. http://dx.doi.org/10.3390/heritage7060141.

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This study concerns the characterization of the color palette of Michelino da Besozzo, one of the leading painters and illuminators of the Late Gothic period in Northern Italy. The artist’s relationship with the color blue was investigated by considering the recipe for lapis lazuli given by the artist to Giovanni Alcherio in Venice in 1410 and found in the medieval treatise of Jean Lebegue. The paper highlights this important evidence for the study of painting technique in the first half of the 15th century with an analytical and technical study of two paintings: The Mystic Marriage of Saint C
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3

Pesaresi, D., M. Romanelli, C. Barnaba, P. L. Bragato, and G. Durì. "OGS improvements in 2012 in running the North-eastern Italy Seismic Network: the Ferrara VBB borehole seismic station." July 22, 2014. https://doi.org/10.5194/adgeo-36-61-2014.

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Abstract. The Centro di Ricerche Sismologiche (CRS, Seismological Research Centre) of the Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS, Italian National Institute for Oceanography and Experimental Geophysics) in Udine (Italy) after the strong earthquake of magnitude M=6.4 occurred in 1976 in the Italian Friuli-Venezia Giulia region, started to operate the North-eastern Italy Seismic Network: it currently consists of 17 very sensitive broad band and 18 simpler short period seismic stations, all telemetered to and acquired in real time at the OGS-CRS data centre in Udine.
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4

Enrico Priolo, Marco Romanelli, Carla Barnaba, et al. "The Ferrara thrust earthquakes of May-June 2012: preliminary site response analysis at the sites of the OGS temporary network." Annals of Geophysics 55, no. 4 (2012). http://dx.doi.org/10.4401/ag-6172.

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<p>Following the Ml 5.9 earthquake that struck the Emilia area in northern Italy on May 20, 2012, at 02:03:53 UTC, and in co-operation with the personnel of the Municipality of Ferrara and the University of Ferrara, a team of seismologists of the Istituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS; National Institute of Oceanography and Experimental Geophysics) deployed a temporary seismographic network. This consisted of eight portable seismological stations, to record the local earthquakes that occurred during the seismic sequence. The OGS intervention was integrated into
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5

Riccardo Caputo, Kyriaki Iordanidou, Luca Minarelli, et al. "Geological evidence of pre-2012 seismic events, Emilia-Romagna, Italy." Annals of Geophysics 55, no. 4 (2012). http://dx.doi.org/10.4401/ag-6148.

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<p>In May 2012, two moderate (-to-strong) earthquakes that were associated with a noticeable aftershock sequence affected the eastern sector of the Po Plain, Italy, in correspondence with a buried portion of the Apennines thrust belt. The Provinces of Ferrara, Modena and Bologna (Emilia Romagna Region), Mantua (Lombardy Region), and Rovigo (Veneto Region) were affected to different extents. The first shock (Ml 5.9 according to the Istituto Nazionale di Geofisica e Vulcanologia (INGV; National Institute of Geophysics and Volcanology), and Mw 6.1 according to the US Geological Service) occ
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6

Andrea Tertulliani, Luca Arcoraci, Michele Berardi, et al. "The Emilia 2012 sequence: a macroseismic survey." Annals of Geophysics 55, no. 4 (2012). http://dx.doi.org/10.4401/ag-6140.

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<p>On May 20, 2012, at 4:03 local time (2:03 UTC), a large part of the Po Valley between the cities of Ferrara, Modena and Mantova was struck by a damaging earthquake (Ml 5.9). The epicenter was located by the Istituto Nazionale di Geo-fisica e Vulcanologia (INGV) seismic network [ISIDe 2010] at 44.889 ˚N and 11.228 ˚E, approximately 30 km west of Ferrara (Figure 1). The event was preceded by a foreshock that occurred at 01:13 local time, with a magnitude of Ml 4. The mainshock started an intense seismic sequence that lasted for weeks, counting more than 2,000 events, six of which had Ml
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7

Christian Bignami, Pierfrancesco Burrato, Valentina Cannelli, et al. "Coseismic deformation pattern of the Emilia 2012 seismic sequence imaged by Radarsat-1 interferometry." Annals of Geophysics 55, no. 4 (2012). http://dx.doi.org/10.4401/ag-6157.

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<p>On May 20 and 29, 2012, two earthquakes of magnitudes 5.9 and 5.8 (Mw), respectively, and their aftershock sequences hit the central Po Plain (Italy), about 40 km north of Bologna. More than 2,000 sizable aftershocks were recorded by the Isti-tuto Nazionale di Geofisica e Vulcanologia (INGV; National Institute of Geophysics and Volcanology) National Seismic Network (http://iside.rm.ingv.it/). The sequence was generated by pure compressional faulting over blind thrusts of the western Ferrara Arc, and it involved a 50-km-long stretch of this buried outer front of the northern Apennines.
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8

"Preface." Journal of Physics: Conference Series 2242, no. 1 (2022): 011001. http://dx.doi.org/10.1088/1742-6596/2242/1/011001.

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Abstract With the successful organizing a series of world-class conferences, and a close cooperation among the University of Messina, Italy; University of Ferrara, Italy; Istituto Nazionale di Fisica Nucleare (INFN); Wuhan University, China, we have been making great efforts to hold the the 2022 First International Conference on Advances in Modern Physics Sciences and Engineering Technology-PSET 2022, which will be happened on March 5-6th 2022, in Beijing, China, organized by Wuhan University, China and Istituto Nazionale di Fisica Nucleare (INFN). 3 sessions are included in PSET22: Applied Ph
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9

"Preface." Journal of Physics: Conference Series 2549, no. 1 (2023): 011001. http://dx.doi.org/10.1088/1742-6596/2549/1/011001.

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The 2nd International Conference on Advances in Modern Physics Sciences and Engineering Technology - PSET 2023 has been held on April 29th-30th, 2023, in Wuhan, China. This conference is organized by the China University of Geosciences (Wuhan), China, and the Istituto Nazionale di Fisica Nucleare (INFN), in collaboration with Wuhan University, China, University of Huddersfield, UK, University of Messina, Italy, and University of Ferrara, Italy. The primary goal of this conference is to provide a platform for presenting the latest advancements and research findings in engineering technology and
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10

Marco Massa, Paolo Augliera, Gianlorenzo Franceschina, Sara Lovati, and Maria Zupo. "The July 17, 2011, ML 4.7, Po Plain (northern Italy) earthquake: strong-motion observations from the RAIS network." Annals of Geophysics 55, no. 2 (2012). http://dx.doi.org/10.4401/ag-5389.

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<p>On July 17, 2011, at 18:30:23 UTC, a M<sub>L</sub> 4.7 earthquake occurred on the east side of the Po Plain (northern Italy), between the towns of Ferrara and Rovigo. The epicentral coordinates provided by the National Earthquake Center of the Istituto Nazionale di Geofisica e Vulcanologia (National Institute of Geophysics and Volcanology, INGV) were 45.01˚N and 11.41˚E (http://iside.rm.ingv.it/iside). The depth of the hypocenter was constrained at 8.1 km, corresponding to a buried active source that existed in the area. The source of the event was characterized by a predo
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Books on the topic "Pinacoteca nazionale (Ferrara, Italy)"

1

Ferrara, Pinacoteca nazionale di, ed. La pinacoteca nazionale di Ferrara: Guida. Franco Cosimo Panini, 2021.

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2

Guerzi, Chiara, and Andrei Bliznukov. Lampi sublimi a Ferrara: Tra Michelangelo e Tiziano, Bastianino e il cantiere di San Paolo. Edizioni Edisai, 2017.

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3

Jadranka, Bentini, and Pinacoteca nazionale di Ferrara, eds. La Pinacoteca nazionale di Ferrara. Nuova alfa editoriale, 1990.

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4

Jadranka, Bentini, and Pinacoteca nazionale di Ferrara, eds. La Pinacoteca nazionale di Ferrara: Catalogo generale. Nuova alfa editoriale, 1992.

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Jadranka, Bentini, and Pinacoteca nazionale di Ferrara, eds. La Pinacoteca nazionale di Ferrara: Guida illustrata. Nuova Alfa editoriale, 1990.

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6

D'Amico, Rosa. The Pinacoteca nazionale of Bologna. Marsilio, 2001.

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7

Jadranka, Bentini, Cammarota Giampiero, and Scaglietti Kelescian Daniela, eds. Pinacoteca nazionale di Bologna: Catalogo generale. Marsilio, 2005.

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8

Baldoni, Daniela. Guida al Museo archeologico nazionale di Ferrara. Ministero per i beni e le attività culturali, Soprintendenza archeologica per i beni archeologici dell'Emilia Romagna, 2001.

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9

Italy), Pinacoteca nazionale (Bologna. Figure: Disegni dal Cinquecento all'Ottocento nella Pinacoteca nazionale di Bologna. Electa, 1998.

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10

Scardino, Lucio. Documenti sulla quadreria Vendeghini-Baldi di Ferrara. Liberty house, 2008.

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