Results 171 to 180 of about 21,388 (221)
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Mucilage impact on gorgonians in the Tyrrhenian sea
Science of The Total Environment, 2005The mucilage phenomenon has affected the Tuscan Archipelago since its first appearance (1991) in the Tyrrhenian Sea (Mediterranean Sea) [Innamorati M, Raddi E, Buzzichelli A, Melley S, Demoulin M. Le mucillaggini nel Mar Tirreno. Biol Mar Suppl Notiz 1992;1:23-26; Sartoni G, Sonni C. Tribonema marinum J.
S, Giuliani +3 more
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Geochemistry of basalts from the Tyrrhenian Sea
Nature, 1979Comparison between the Tyrrhenian basalts and oceanic basalts coming from different geodynamic environments shows that Tyrrhenian basalts have a clear organic signature with a transitional character.
Bruno Hamelin +4 more
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Geothermal structure of the Tyrrhenian Sea
Marine Geology, 1984Over 200 heat flow measurements have been carried out in the Tyrrhenian Sea, mostly since 1977 as part of the “Heat Flow Map for Italy and Surrounding Seas” Italian program, as well as part of the French—Italian “Tyrrhenia” program. All data have been corrected for the influence of the Plio-Quaternary sedimentation. Measured heat flow values were
DELLA VEDOVA, BRUNO +3 more
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2012
The Tyrrhenian Sea is the easternmost basin of the western Mediterranean boudinated backarc lithosphere (where the Provençal, Valencia, and Algerian troughs also developed) in the hanging wall of the Late Oligocene to Present Apennines-Maghrebides subduction.
Scrocca D +5 more
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The Tyrrhenian Sea is the easternmost basin of the western Mediterranean boudinated backarc lithosphere (where the Provençal, Valencia, and Algerian troughs also developed) in the hanging wall of the Late Oligocene to Present Apennines-Maghrebides subduction.
Scrocca D +5 more
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The Deep Seismicity of the Tyrrhenian Sea*
Terra Nova, 1991AbstractThe deep seismicity of the Tyrrhenian Sea is analysed using data from a new instrumental catalogue of the seismicity of the Italian area. We use algorithms for the determination of absolute and relative hypocentral locations and for the evaluation of the geometry and coherence of the state of stress within the subducting slab.
Domenico Giardini, Maddalena Velonà
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2016
The Southern Tyrrhenian seafloor (south of the 41° Parallel line) hosts a large number of Miocene to Quaternary volcanoes ranging in composition from MORB- to OIB- and arc-type. MORB-type rocks are concentrated in the Vavilov Basin, but their role is evident for other Tyrrhenian Sea volcanoes.
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The Southern Tyrrhenian seafloor (south of the 41° Parallel line) hosts a large number of Miocene to Quaternary volcanoes ranging in composition from MORB- to OIB- and arc-type. MORB-type rocks are concentrated in the Vavilov Basin, but their role is evident for other Tyrrhenian Sea volcanoes.
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The Tyrrhenian Sea and Adjoining Regions
1978The Tyrrhenian Sea, in the central Mediterranean area, is bounded on the northern and eastern sides by the Italian Peninsula, and on the western and southern sides by the Ligurian Sea, Corsica, Sardinia, and Sicily. It covers a triangular area of 231,000 km2 (Carter et al., 1972) and reaches a maximum depth of 3620 m (Selli, 1970a).
M. Boccaletti, P. Manetti
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Thermohaline staircase formations in the Tyrrhenian Sea
Deep Sea Research Part I: Oceanographic Research Papers, 1996Hydrographic measurements taken in the Tyrrhenian Sea in two different seasons revealed well pronounced thermohaline stepped structures lying between the Levantine Intermediate Water (LIW) and the Deep Water (DW). The investigated staircase, found in the depth range of 600–2500 m, was composed of four to eight homogeneous layers, each about 20–54 m ...
George Zodiatis, Gian Pietro Gasparini
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Extreme wave conditions in the tyrrhenian sea
Ocean Engineering, 1986A hindcast study of extreme wave conditions in the Tyrrhenian Sea is described. The paper covers the different steps of the work, including the identification and the statistics of the weather patterns in the area, the choice of the storms to be hindcasted, the wind and wave models, a check of the best extremal distributions for the estimate of the ...
L. Cavaleri +4 more
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Saharan dust incursion over the Tyrrhenian Sea
Atmospheric Environment (1967), 1984Abstract The Tyrrhenian Sea aerosol was sampled by both mesh and filter techniques. Geostrophic back trajectories were used to identify potential aerosol catchment regions, and it was shown that the atmosphere over the Tyrrhenian Sea received incursions of Saharan dust during the collection period in the autumn of 1979.
R. Chester +3 more
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