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all geography including DSDP/ODP Sites and Legs
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Africa
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Europe
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Malta (1)
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Mediterranean Sea
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Strait of Sicily (16)
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oxygen
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ocean-island basalts (1)
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trachytes (2)
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Invertebrata
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Fusulinina
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Archaediscidae (1)
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Rotaliina
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Buliminacea (1)
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isotopes
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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stable isotopes
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Nd-144/Nd-143 (2)
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O-18/O-16 (1)
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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Sr-87/Sr-86 (2)
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lava (2)
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mantle (2)
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Mediterranean Sea
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Ionian Sea (1)
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Strait of Sicily (16)
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West Mediterranean
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Ligurian Sea (1)
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Tyrrhenian Sea (1)
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Mesozoic
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Triassic (1)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (2)
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lead
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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rare earths
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neodymium
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metasomatism (1)
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Ocean Drilling Program
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Leg 160
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ODP Site 963 (1)
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ocean floors (3)
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Emiliania
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Strait of Sicily
Collating European data on geological events in submerged areas: examples of correlation and interpretation from Italian seas Available to Purchase
Abstract The European Marine Observation and Data Network (EMODnet) Project provides freely available data on European seas. The main purpose of EMODnet is to overcome the fragmentation and dishomogeneity of the available data, providing access to a harmonized and interoperable database. The EMODnet Geology Lot includes information at multiple scales on the seabed and its substrate ( http://www.emodnet-geology.eu/ ). The dataset on ‘Geological events and probabilities’ collects information on landslides, earthquakes, volcanic structures, active tectonics, tsunamis and fluid emissions. The Geological Survey of Italy, which coordinates the collation of ‘Geological events and probabilities’ data, provided guidelines to compile layers complemented by comprehensive and detailed patterns of attributes for each feature in order to characterize each type of geological event. Occurrences of events are often associated with each other, particularly in tectonically active areas. Geological events affect both submerged and coastal environments. Data gathered by EMODnet Geology provide a good basis for further studies, contributing to the outlining of different tectonic settings and providing support to the use of marine resources, as well as to the management of marine-coastal areas particularly regarding the identification and assessment of geological and environmental hazards.
Neogene stratigraphic evolution of a tectonically controlled continental shelf: the example of the Lampedusa Island Available to Purchase
New insights on the tectonics of the Lampedusa Plateau from the integration of offshore, on-land and space geodetic data Available to Purchase
Paleomagnetism of the Hyblean Plateau, Sicily: a review of the existing data set and new evidence for lack of block rotation from the Scicli-Ragusa Fault System Available to Purchase
Anatomy of a submerged archipelago in the Sicilian Channel (central Mediterranean Sea) Available to Purchase
A Mediterranean petroleum province on the North Africa Plate margin: The Sicily Channel Available to Purchase
Distribution of faults and extensional strain in fractured carbonates of the North Malta Graben Available to Purchase
Origin and evolution of the Pleistocene magmatism of Linosa Island (Sicily Channel, Italy) Available to Purchase
Petrology and Geochemistry of Submarine Volcanism in the Sicily Channel Rift Available to Purchase
Coexisting geodynamic processes in the Sicily Channel Available to Purchase
The northwestern side of the Sicily Channel in the central Mediterranean has been shaped by the occurrence of two independent tectonic processes that overlap each other, the Maghrebides-Apennines accretionary prism and the Sicily Channel rift. Since at least the Pliocene, these two processes have acted simultaneously, being respectively related to the Apennines subduction and to the African rift. Thrust sheets of the accretionary prism crosscut the almost orthogonal rift-related normal faults and vice versa. Analog modeling supports the kinematics inferred from regional structural data. Alkaline magmatism associated with the rift is more pronounced in the foreland of the prism, where the extension is more concentrated. This peculiar setting confirms how independently geodynamic processes can interact in the same area at the same time, suggesting that plate boundaries are passive features responding to far-field velocity fields of the lithosphere.