Littérature scientifique sur le sujet « Apennine chain »

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Articles de revues sur le sujet "Apennine chain"

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Rapisarda, F. "Landslide analysis in Apennine chain areas." Landslides 4, no. 1 (2007): 75–83. http://dx.doi.org/10.1007/s10346-006-0066-8.

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Zanchetta, Giovanni, Carlo Giraudi, Roberto Sulpizio, Michel Magny, Russell N. Drysdale, and Laura Sadori. "Constraining the onset of the Holocene “Neoglacial” over the central Italy using tephra layers." Quaternary Research 78, no. 2 (2012): 236–47. http://dx.doi.org/10.1016/j.yqres.2012.05.010.

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AbstractA study of six tephra layers discovered in different deposits between 1600 and 2700 m a.s.l. in the Apennine chain in central Italy allowed precise stratigraphic constraints on environmental and climatic changes between ca. 4.5 and 3.8 cal ka BP. Chemical analyses allowed the correlation of these tephra layers with the eruptions of Agnano Mt Spina (AMST) from Phlegrean Field and Avellino (AVT) from Somma–Vesuvius. Major environmental changes in the high mountains of the Central Apennines occurred just after the deposition of the AMST and predate the deposition of the AVT. At this time,
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Mele, G. "Pn Anisotropy in the Northern Apennine Chain (Italy)." Pure and Applied Geophysics 151, no. 2-4 (1998): 495–502. http://dx.doi.org/10.1007/s000240050125.

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Gori, Stefano, Emanuela Falcucci, Chiara Ladina, Simone Marzorati, and Fabrizio Galadini. "Active faulting, 3-D geological architecture and Plio-Quaternary structural evolution of extensional basins in the central Apennine chain, Italy." Solid Earth 8, no. 2 (2017): 319–37. http://dx.doi.org/10.5194/se-8-319-2017.

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Abstract. The general basin and range Apennine topographic characteristic is generally attributed to the presently active normal fault systems, whose long-term activity (throughout the Quaternary) is supposed to have been responsible for the creation of morphological/structural highs and lows. By coupling field geological survey and geophysical investigations, we reconstructed the 3-D geological model of an inner tectonic basin of the central Apennines, the Subequana Valley, bounded to the northeast by the southern segment of one of the major active and seismogenic normal faults of the Apennin
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Bartolini, C. "When did the Northern Apennine become a mountain chain?" Quaternary International 101-102 (January 2003): 75–80. http://dx.doi.org/10.1016/s1040-6182(02)00090-3.

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Turco, Eugenio, Chiara Macchiavelli, Giulia Penza, Antonio Schettino, and Pietro Paolo Pierantoni. "Kinematics of Deformable Blocks: Application to the Opening of the Tyrrhenian Basin and the Formation of the Apennine Chain." Geosciences 11, no. 4 (2021): 177. http://dx.doi.org/10.3390/geosciences11040177.

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We describe the opening of back-arc basins and the associated formation of accretionary wedges through the application of techniques of deformable plate kinematics. These methods have proven to be suitable to describe complex tectonic processes, such as those that are observed along the Africa–Europe collision belt. In the central Mediterranean area, these processes result from the passive subduction of the lithosphere belonging to the Alpine Tethys and Ionian Ocean. In particular, we focus on the opening of the Tyrrhenian basin and the contemporary formation of the Apennine chain. We divide t
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Schiattarella, Marcello, Salvatore Ivo Giano, and Dario Gioia. "Long-term geomorphological evolution of the axial zone of the Campania-Lucania Apennine, southern Italy: a review." Geologica Carpathica 68, no. 1 (2017): 57–67. http://dx.doi.org/10.1515/geoca-2017-0005.

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Abstract Uplift and erosion rates have been calculated for a large sector of the Campania-Lucania Apennine and Calabrian arc, Italy, using both geomorphological observations (elevations, ages and arrangement of depositional and erosional land surfaces and other morphotectonic markers) and stratigraphical and structural data (sea-level related facies, base levels, fault kinematics, and fault offset estimations). The values of the Quaternary uplift rates of the southern Apennines vary from 0.2 mm/yr to about 1.2–1.3 mm/yr. The erosion rates from key-areas of the southern Apennines, obtained from
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Mongelli, F., G. Zito, N. Ciaranfi, and P. Pieri. "Interpretation of heat flow density of the Apennine chain, Italy." Tectonophysics 164, no. 2-4 (1989): 267–80. http://dx.doi.org/10.1016/0040-1951(89)90020-6.

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Lapenna, V., M. Macchiato, S. Piscitelli, and L. Telesca. "Scale-invariance Properties in Seismicity of Southern Apennine Chain (Italy)." Pure and Applied Geophysics 157, no. 4 (2000): 589–601. http://dx.doi.org/10.1007/pl00001109.

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Di Toro, Francesco, Gianmarco Minuti, Luca Coppari, et al. "Rana temporaria on Monti della Laga (Central Italy): isolated population or wide distribution? First record in Abruzzo and Marche." Acta Herpetologica 16, no. 1 (2021): 45–51. http://dx.doi.org/10.36253/a_h-9824.

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In Central Italy Rana temporaria is only known to occur as a glacial relict on the eastern side of Monti della Laga (Lazio). In this study we report the presence of the species in other areas of the mountain chain, with documented sightings in five distinct localities in Marche and Abruzzo. We use these new records, together with other occurrence data from the Apennine chain, to generate a species distribution model and perform an analysis of the geological preference of the species in Central Italy. Although the model indicates a wide area of Marche and Abruzzo as suitable for R. temporaria,
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Chapitres de livres sur le sujet "Apennine chain"

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Mele, Giuliana. "Pn Anisotropy in the Northern Apennine Chain (Italy)." In Geodynamics of Lithosphere & Earth’s Mantle. Birkhäuser Basel, 1998. http://dx.doi.org/10.1007/978-3-0348-8777-9_14.

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Lapenna, V., M. Macchiato, S. Piscitelli, and L. Telesca. "Scale-invariance Properties in Seismicity of Southern Apennine Chain (Italy)." In Fractals and Dynamic Systems in Geoscience. Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-8430-3_7.

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Minzoni, Nello. "Characteristics of the circum-Tyrrhenian Hercynian massifs and their role in the Alpine-Apennine chains." In Proceedings of the International Conferences on Basement Tectonics. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-1614-5_38.

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Woodhouse, Barbara Bennett. "A Tale of Two Villages." In The Ecology of Childhood. NYU Press, 2020. http://dx.doi.org/10.18574/nyu/9780814794845.003.0003.

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Chapter three opens with detailed the two villages that are compared in this book, Scanno Italy and Cedar Key Florida. The portraits cover demography, history, political structure, geography, natural surroundings, social customs and traditions, with a particular focus on the lives of children. Both communities serve populations hovering around 1,700; both are majority Caucasian; both have strong community identities and traditions; and both are located in remote natural environments, with Scanno tucked in a valley of the Apennine Mountains in the Abruzzo region of Central Italy and Cedar Key occupying a chain of islands on the sparsely settled Gulf Coast of Florida in the South of the United States. The village portraits are followed by explicit comparisons of similarities and differences that are most relevant to the ecology of childhood, including early childhood and education systems, access to free play spaces, living on the edge of natural disaster, children’s sense of history and place, economic trauma and resilience, and presence or absence of racial and ethnic tension. The chapter closes with an exercise in triangulation, using multiple sources and uncomfortable conversations to explore attitudes towards racial and ethnic diversity.
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Enrico, Miccadei, and Piacentini Tommaso. "Two Tectonic Geomorphology Studies on the Landscape and Drainage Network of Chain and Piedmont Areas of the Abruzzi Region (Central Apennines, Italy)." In New Frontiers in Tectonic Research - At the Midst of Plate Convergence. InTech, 2011. http://dx.doi.org/10.5772/18969.

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Actes de conférences sur le sujet "Apennine chain"

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Esestime, P., W. Paltrinieri, and F. Calamita. "The Apulian Chain, Buried Below the Southern Apennines Allochthonous Units (Italy)." In 72nd EAGE Conference and Exhibition incorporating SPE EUROPEC 2010. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609.201401075.

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