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Hydrocarbons plays and prospectivity of the Mediterranean ridge

Manoutsoglou Emmanouil, Pantopoulos, G, Makrodimitras ,G, Konstantopoulos Panagiotis

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URIhttp://purl.tuc.gr/dl/dias/3EB792F4-0179-4753-8BE1-9195CF4D7055-
Identifierhttps://doi.org/10.1080/15567036.2011.582600-
Languageen-
Extent9 pagesen
TitleHydrocarbons plays and prospectivity of the Mediterranean ridge en
CreatorManoutsoglou Emmanouilen
CreatorΜανουτσογλου Εμμανουηλel
CreatorPantopoulos, Gen
Creator Makrodimitras ,Gen
CreatorKonstantopoulos Panagiotisen
CreatorΚωνσταντοπουλος Παναγιωτηςel
PublisherTaylor & Francisen
Content SummaryThe Mediterranean Ridge, the largest physiographic feature in the Eastern Mediterranean Sea, is thought to be an accretionary complex, resulting from the convergence of the African and Eurasian plates. The presence of a salt layer in the upper deforming sequence (Late Miocene evaporites) and the unusually great thickness of the incoming sediment column differentiate the Mediterranean Ridge from most other accretionary complexes. Mud volcanoes are present in this region while various lithotypes from Carboniferous to Pleistocene can act as potential source, reservoir, and seal rocks resulting to the recognition of several potential hydrocarbon plays.en
Type of ItemPeer-Reviewed Journal Publicationen
Type of ItemΔημοσίευση σε Περιοδικό με Κριτέςel
Licensehttp://creativecommons.org/licenses/by/4.0/en
Date of Item2015-10-29-
Date of Publication2015-
SubjectHydrocarbonsen
Bibliographic CitationA. Maravelis , E. Manutsoglou ,P. Konstantopoulos , G. Pantopoulos , G. Makrodimitras , E. Zoumpoulis , A. Zelilidis ,"Hydrocarbons plays and prospectivity of the Mediterranean ridge,"En. Sour. Part A,vol. 37,no.4 ,pp.347-355,Jan. 2015.doi: 10.1080/15567036.2011.582600 en

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