The tectonics of the eastern Mediterranean: A geophysical review
Identifieur interne : 000570 ( Main/Exploration ); précédent : 000569; suivant : 000571The tectonics of the eastern Mediterranean: A geophysical review
Auteurs : J. M. LortSource :
- Reviews of Geophysics [ 8755-1209 ] ; 1971-05.
Descripteurs français
- Wicri :
- geographic : Chypre (pays).
- topic : Crète.
English descriptors
- KwdEn :
- Adriatic, Aegean plate, African plate, Allan, Anomaly, Anticlockwise rotation, Apulian plate, Balearic, Balearic basin, Basin, Bouguer anomalies, Calabrian island, Central basin, Contoured maps, Counterclockwise rotation, Crete, Crete island, Crust, Crustal, Crustal destruction, Crustal structure, Cyprus, Eastern mediterranean, Eastern mediterranean tectonics, Eastern mediterraneansea, European plates, Ewing, Geol, Geological observatory, Goncharovand mikhaylov, Gravity anomalies, Gravity anomaliesof, Heat flow, Heezen, Hellenic trough, Hersey, Higgs, Inner trench, Ligurian, Ligurian trough, Lines enclose, Lort, Magnetic stripes, Mediterranean, Mediterranean basin, Mediterranean region, Mediterranean ridge, Mediterranean tectonics, Mediterranean trough, Morelli, Naval oceanographicoffice, Oceanic, Oceanic crust, Physiographic provinces, Plate tectonics, Refraction, Refraction data, Relative motions, Saclant center, Sediment, Sediment deformation, Seismic, Seismic activity, Seismicity, Southern margin, Tectonic, Tectonic history, Tectonics, Trans, Trench, Tyrrhenian, Tyrrhenian basins, Underthrusting, Unpublished, Unpublished data, Unpublished manuscript, Vogt, Western mediterranean, Whole region, Woods hole oceanographicinstitution.
- Teeft :
- Adriatic, Aegean plate, African plate, Allan, Anomaly, Anticlockwise rotation, Apulian plate, Balearic, Balearic basin, Basin, Bouguer anomalies, Calabrian island, Central basin, Contoured maps, Counterclockwise rotation, Crete, Crete island, Crust, Crustal, Crustal destruction, Crustal structure, Cyprus, Eastern mediterranean, Eastern mediterranean tectonics, Eastern mediterraneansea, European plates, Ewing, Geol, Geological observatory, Goncharovand mikhaylov, Gravity anomalies, Gravity anomaliesof, Heat flow, Heezen, Hellenic trough, Hersey, Higgs, Inner trench, Ligurian, Ligurian trough, Lines enclose, Lort, Magnetic stripes, Mediterranean, Mediterranean basin, Mediterranean region, Mediterranean ridge, Mediterranean tectonics, Mediterranean trough, Morelli, Naval oceanographicoffice, Oceanic, Oceanic crust, Physiographic provinces, Plate tectonics, Refraction, Refraction data, Relative motions, Saclant center, Sediment, Sediment deformation, Seismic, Seismic activity, Seismicity, Southern margin, Tectonic, Tectonic history, Tectonics, Trans, Trench, Tyrrhenian, Tyrrhenian basins, Underthrusting, Unpublished, Unpublished data, Unpublished manuscript, Vogt, Western mediterranean, Whole region, Woods hole oceanographicinstitution.
Abstract
A summary is given of present geophysical data available for the eastern Mediterranean, and the structural and tectonic history of the area is interpreted. The western Mediterranean is described in sufficient detail only for comparison. The region is delineated into plates on the basis of seismic activity at their margins. The African plate is moving northward relative to Europe with crustal destruction and underthrusting occurring along the Crete and Calabrian island arc systems. The intervening Aegean, Apulian, and Turkish plates are small and rapidly moving; they show intense seismicity at the boundaries. All observations (sediment deformation, gravity, magnetics and heat flow) suggest the existence of a zone of compression in the eastern Mediterranean. Anticlockwise rotation relative to Eurasia of parts of southern Europe occurred during an extensional phase in the west, permitting the development of new oceanic crust and accompanied by compression in the east. What little evidence there is suggests that the crust in the eastern Mediterranean is oceanic, but there are no magnetic stripes to indicate the orientation of the mid‐oceanic ridge from which it developed.
Url:
DOI: 10.1029/RG009i002p00189
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 000447
- to stream Istex, to step Curation: 000447
- to stream Istex, to step Checkpoint: 000486
- to stream Main, to step Merge: 000593
- to stream Main, to step Curation: 000570
Le document en format XML
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<term>Aegean plate</term>
<term>African plate</term>
<term>Allan</term>
<term>Anomaly</term>
<term>Anticlockwise rotation</term>
<term>Apulian plate</term>
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<term>Balearic basin</term>
<term>Basin</term>
<term>Bouguer anomalies</term>
<term>Calabrian island</term>
<term>Central basin</term>
<term>Contoured maps</term>
<term>Counterclockwise rotation</term>
<term>Crete</term>
<term>Crete island</term>
<term>Crust</term>
<term>Crustal</term>
<term>Crustal destruction</term>
<term>Crustal structure</term>
<term>Cyprus</term>
<term>Eastern mediterranean</term>
<term>Eastern mediterranean tectonics</term>
<term>Eastern mediterraneansea</term>
<term>European plates</term>
<term>Ewing</term>
<term>Geol</term>
<term>Geological observatory</term>
<term>Goncharovand mikhaylov</term>
<term>Gravity anomalies</term>
<term>Gravity anomaliesof</term>
<term>Heat flow</term>
<term>Heezen</term>
<term>Hellenic trough</term>
<term>Hersey</term>
<term>Higgs</term>
<term>Inner trench</term>
<term>Ligurian</term>
<term>Ligurian trough</term>
<term>Lines enclose</term>
<term>Lort</term>
<term>Magnetic stripes</term>
<term>Mediterranean</term>
<term>Mediterranean basin</term>
<term>Mediterranean region</term>
<term>Mediterranean ridge</term>
<term>Mediterranean tectonics</term>
<term>Mediterranean trough</term>
<term>Morelli</term>
<term>Naval oceanographicoffice</term>
<term>Oceanic</term>
<term>Oceanic crust</term>
<term>Physiographic provinces</term>
<term>Plate tectonics</term>
<term>Refraction</term>
<term>Refraction data</term>
<term>Relative motions</term>
<term>Saclant center</term>
<term>Sediment</term>
<term>Sediment deformation</term>
<term>Seismic</term>
<term>Seismic activity</term>
<term>Seismicity</term>
<term>Southern margin</term>
<term>Tectonic</term>
<term>Tectonic history</term>
<term>Tectonics</term>
<term>Trans</term>
<term>Trench</term>
<term>Tyrrhenian</term>
<term>Tyrrhenian basins</term>
<term>Underthrusting</term>
<term>Unpublished</term>
<term>Unpublished data</term>
<term>Unpublished manuscript</term>
<term>Vogt</term>
<term>Western mediterranean</term>
<term>Whole region</term>
<term>Woods hole oceanographicinstitution</term>
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<term>Aegean plate</term>
<term>African plate</term>
<term>Allan</term>
<term>Anomaly</term>
<term>Anticlockwise rotation</term>
<term>Apulian plate</term>
<term>Balearic</term>
<term>Balearic basin</term>
<term>Basin</term>
<term>Bouguer anomalies</term>
<term>Calabrian island</term>
<term>Central basin</term>
<term>Contoured maps</term>
<term>Counterclockwise rotation</term>
<term>Crete</term>
<term>Crete island</term>
<term>Crust</term>
<term>Crustal</term>
<term>Crustal destruction</term>
<term>Crustal structure</term>
<term>Cyprus</term>
<term>Eastern mediterranean</term>
<term>Eastern mediterranean tectonics</term>
<term>Eastern mediterraneansea</term>
<term>European plates</term>
<term>Ewing</term>
<term>Geol</term>
<term>Geological observatory</term>
<term>Goncharovand mikhaylov</term>
<term>Gravity anomalies</term>
<term>Gravity anomaliesof</term>
<term>Heat flow</term>
<term>Heezen</term>
<term>Hellenic trough</term>
<term>Hersey</term>
<term>Higgs</term>
<term>Inner trench</term>
<term>Ligurian</term>
<term>Ligurian trough</term>
<term>Lines enclose</term>
<term>Lort</term>
<term>Magnetic stripes</term>
<term>Mediterranean</term>
<term>Mediterranean basin</term>
<term>Mediterranean region</term>
<term>Mediterranean ridge</term>
<term>Mediterranean tectonics</term>
<term>Mediterranean trough</term>
<term>Morelli</term>
<term>Naval oceanographicoffice</term>
<term>Oceanic</term>
<term>Oceanic crust</term>
<term>Physiographic provinces</term>
<term>Plate tectonics</term>
<term>Refraction</term>
<term>Refraction data</term>
<term>Relative motions</term>
<term>Saclant center</term>
<term>Sediment</term>
<term>Sediment deformation</term>
<term>Seismic</term>
<term>Seismic activity</term>
<term>Seismicity</term>
<term>Southern margin</term>
<term>Tectonic</term>
<term>Tectonic history</term>
<term>Tectonics</term>
<term>Trans</term>
<term>Trench</term>
<term>Tyrrhenian</term>
<term>Tyrrhenian basins</term>
<term>Underthrusting</term>
<term>Unpublished</term>
<term>Unpublished data</term>
<term>Unpublished manuscript</term>
<term>Vogt</term>
<term>Western mediterranean</term>
<term>Whole region</term>
<term>Woods hole oceanographicinstitution</term>
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<keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Chypre (pays)</term>
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<front><div type="abstract">A summary is given of present geophysical data available for the eastern Mediterranean, and the structural and tectonic history of the area is interpreted. The western Mediterranean is described in sufficient detail only for comparison. The region is delineated into plates on the basis of seismic activity at their margins. The African plate is moving northward relative to Europe with crustal destruction and underthrusting occurring along the Crete and Calabrian island arc systems. The intervening Aegean, Apulian, and Turkish plates are small and rapidly moving; they show intense seismicity at the boundaries. All observations (sediment deformation, gravity, magnetics and heat flow) suggest the existence of a zone of compression in the eastern Mediterranean. Anticlockwise rotation relative to Eurasia of parts of southern Europe occurred during an extensional phase in the west, permitting the development of new oceanic crust and accompanied by compression in the east. What little evidence there is suggests that the crust in the eastern Mediterranean is oceanic, but there are no magnetic stripes to indicate the orientation of the mid‐oceanic ridge from which it developed.</div>
</front>
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