Results 181 to 190 of about 33,895 (245)
Almost billfish: convergent longirostry, micro-dentition, and possible glandular sinuses in a large teleost fish from the Upper Cretaceous of Northern Italy. [PDF]
J AnatSerafini G +5 more
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Rendiconti Online della Società Geologica Italiana, 2013
In the Southern Apennines and Calabria outcrop metamorphic slices of hercynian and/or alpine age. The reconstructions by Glauco Bonardi and co-authors of an alpine subduction-related origin for the emplacement of those rocks is still supported by a number of tectonic and geodynamic constraints.
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In the Southern Apennines and Calabria outcrop metamorphic slices of hercynian and/or alpine age. The reconstructions by Glauco Bonardi and co-authors of an alpine subduction-related origin for the emplacement of those rocks is still supported by a number of tectonic and geodynamic constraints.
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2001
The Northern Apennines are a fold—thrust belt formed during the Tertiary by the tectonic superposition from W to E of the Ligurides on the Tuscan nappe and on the Tuscan metamorphic complex (Boccaletti et al., 1971; Alvarez et al., 1974; Kligfield, 1979). The ophiolite-bearing Ligurides derived from the southern extension of the Ligurian—Piedmont ocean,
Luigi Carmignani +7 more
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The Northern Apennines are a fold—thrust belt formed during the Tertiary by the tectonic superposition from W to E of the Ligurides on the Tuscan nappe and on the Tuscan metamorphic complex (Boccaletti et al., 1971; Alvarez et al., 1974; Kligfield, 1979). The ophiolite-bearing Ligurides derived from the southern extension of the Ligurian—Piedmont ocean,
Luigi Carmignani +7 more
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2001
The outer Northern Apennines (ONA) are an arc-shaped fold-and-thrust belt, with northeastward convexity and vergence, that plunges northwestward, extending through Romagna and Umbria—Marche to northern Latium. From the SW to the NE, it is situated between the inner Northern Apennines and the Po Plain—Adriatic foreland.
BARCHI, Massimiliano Rinaldo +3 more
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The outer Northern Apennines (ONA) are an arc-shaped fold-and-thrust belt, with northeastward convexity and vergence, that plunges northwestward, extending through Romagna and Umbria—Marche to northern Latium. From the SW to the NE, it is situated between the inner Northern Apennines and the Po Plain—Adriatic foreland.
BARCHI, Massimiliano Rinaldo +3 more
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Alps-Apennines and Po Plain-frontal Apennines relations
2001The objectives of this chapter are (1) to review the complex relations between the Alps and the Northern Apennines, and (2) to outline the kinematic history in the transitional belt from the Northern Apennines front to the adjoining Po Plain foreland.
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Aftershock Patterns in Recent Central Apennines Sequences
Journal of Geophysical Research: Solid Earth, 2019AbstractDuring the last 20 years, three seismic sequences affected the Apenninic belt (central Italy): Colfiorito (1997–1998), L'Aquila (2009), and Amatrice Visso‐Norcia Campotosto (2016–2017). They lasted for a long time, with a series of moderate‐to‐large earthquakes distributed over 40‐ to 60‐km‐long Apenninic‐trending segments.
G. Sebastiani, A. Govoni, L. Pizzino
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Focal mechanism in the Apennines
Physics and Chemistry of the Earth, 1996Abstract This paper compares different source mechanism models that fit first onset amplitudes for a set of seismic events that occurred in the Apennines, Italy. We selected earthquakes of magnitude greater than 1.0 that match the criteria of appropriate instrumental coverage of the epicentral area, low localisation errors and high signal-to-noise ...
R. Rosini, F. Di Luccio, S. Barba
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Abstract Apennine Crossings follows a modern mountain route across Italy: that of the ‘Great Apennine Excursion’, while moving back and forth in time, from the Middle Ages to the Second World War and from pilgrims merchants and tourists to soldiers, partisans, and poets.
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