Mediterranean Ridge accretionary complex

E1004657

The Mediterranean Ridge accretionary complex is a vast submarine geological structure in the eastern Mediterranean formed by the ongoing convergence and subduction of tectonic plates, resulting in intense deformation and sediment accumulation.

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Statements (48)

Predicate Object
instanceOf accretionary complex
submarine geological structure
tectonic feature
activity tectonically active
age Cenozoic
associatedWith Hellenic arc NERFINISHED
Hellenic trench NERFINISHED
Mediterranean subduction zone NERFINISHED
fluid seepage
gas hydrates
mud volcanoes
seismic activity in eastern Mediterranean
boundedBy Hellenic trench to the north
Libyan–Egyptian continental margin to the south
composition pelagic sediments
thick marine sedimentary sequences
turbidites
countryOffshoreFrom Cyprus NERFINISHED
Egypt NERFINISHED
Greece NERFINISHED
Libya NERFINISHED
extendsFrom south of Crete
extendsTo towards the Cyrenaica margin of North Africa
towards the Levant Basin
formedBy convergence of African Plate and Eurasian Plate
sediment accretion
subduction of African Plate beneath Eurasian Plate
growthMechanism frontal accretion
offscraping of sediments from African Plate
ongoing sediment accretion
influences bathymetry of eastern Mediterranean Sea
sediment transport pathways in eastern Mediterranean
locatedIn Mediterranean Sea
eastern Mediterranean Sea NERFINISHED
overlies subducting African Plate lithosphere
partOf Hellenic subduction system NERFINISHED
process folding
intense deformation of sediments
sediment underplating
thrust faulting
researchMethod deep-sea drilling
multibeam bathymetry
seismic reflection profiling
studiedInDiscipline geophysics
marine geology
tectonics
tectonicSetting convergent plate boundary
trend generally east–west

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Cyprus microplate relatedTo Mediterranean Ridge accretionary complex