The Mediterranean area represents a composite geological puzzle where several different sized microplates are interposed between the two main plates of Eurasia and Africa. These microplates, consisting of both continental and oceanic lithosphere, have been involved in a long-lasting geodynamic history since Early Triassic, the reconstruction of which is still matter of debate. Useful constraints for the geodynamic reconstruction are provided by the study of the on-land remnants of the oceanic lithosphere, i.e. ophiolites, presently preserved in the Alpine collisional belts throughout the whole Mediterranean area. Ophiolites preserve the records of the whole history from continental rifting to sea-floor spreading of the oceanic basins. The rifting and opening of the oceanic basins and their related geodynamic environments, as well as the spreading phases and subsequent closure processes, can be fully investigated by studying ophiolites with different approaches, including petrology, geochemistry, tectonics, stratigraphy, and structural geology. The study of Mediterranean ophiolites is also particularly relevant for providing important constraints for the knowledge of mantle and crustal processes active in modern oceanic lithosphere. The explorations of the present-day oceanic crust, as well as the three-dimensional relationships among different rock units, can be greatly improved by the observation of the internal architecture of well-preserved ophiolite sequences. The G.L.O.M. – Gruppo di Lavoro sulle Ofioliti Mediterranee (Working Group on Mediterranean ophiolites), composed of several Italian researchers having distinct scientific background, has been devoted to the study of the ophiolites in the Mediterranean area since the 70s. Its activity is mainly supported by M.I.U.R. (Ministry of Education, University and Scientific Research) and CNR (National Research Council). In the last years, different teams of Italian researchers have been involved in the studies of ophiolitic sequences from Dinaric-Hellenic and Alpine-Apennine belts, providing a great amount of geological, petrological, geochemical and structural data to the international scientific community. This volume of OFIOLITI includes some selected papers on Mediterranean ophiolites, concerning both original updated syntheses of ongoing research projects and reviews of previous works. This volume will be issued for the International Geological Congress, which will be held in Florence in August 2004. The aim is to present the current knowledge resulting from the Italian research on Mediterranean ophiolites. This volume will be a selected collection from the much larger set of contributions that will be presented at the Congress.

Italian researches on mediterranean ophiolites: Selected contributions

BECCALUVA, Luigi;SACCANI, Emilio;
2004

Abstract

The Mediterranean area represents a composite geological puzzle where several different sized microplates are interposed between the two main plates of Eurasia and Africa. These microplates, consisting of both continental and oceanic lithosphere, have been involved in a long-lasting geodynamic history since Early Triassic, the reconstruction of which is still matter of debate. Useful constraints for the geodynamic reconstruction are provided by the study of the on-land remnants of the oceanic lithosphere, i.e. ophiolites, presently preserved in the Alpine collisional belts throughout the whole Mediterranean area. Ophiolites preserve the records of the whole history from continental rifting to sea-floor spreading of the oceanic basins. The rifting and opening of the oceanic basins and their related geodynamic environments, as well as the spreading phases and subsequent closure processes, can be fully investigated by studying ophiolites with different approaches, including petrology, geochemistry, tectonics, stratigraphy, and structural geology. The study of Mediterranean ophiolites is also particularly relevant for providing important constraints for the knowledge of mantle and crustal processes active in modern oceanic lithosphere. The explorations of the present-day oceanic crust, as well as the three-dimensional relationships among different rock units, can be greatly improved by the observation of the internal architecture of well-preserved ophiolite sequences. The G.L.O.M. – Gruppo di Lavoro sulle Ofioliti Mediterranee (Working Group on Mediterranean ophiolites), composed of several Italian researchers having distinct scientific background, has been devoted to the study of the ophiolites in the Mediterranean area since the 70s. Its activity is mainly supported by M.I.U.R. (Ministry of Education, University and Scientific Research) and CNR (National Research Council). In the last years, different teams of Italian researchers have been involved in the studies of ophiolitic sequences from Dinaric-Hellenic and Alpine-Apennine belts, providing a great amount of geological, petrological, geochemical and structural data to the international scientific community. This volume of OFIOLITI includes some selected papers on Mediterranean ophiolites, concerning both original updated syntheses of ongoing research projects and reviews of previous works. This volume will be issued for the International Geological Congress, which will be held in Florence in August 2004. The aim is to present the current knowledge resulting from the Italian research on Mediterranean ophiolites. This volume will be a selected collection from the much larger set of contributions that will be presented at the Congress.
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/11392/523353
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