URI | http://purl.tuc.gr/dl/dias/3EB792F4-0179-4753-8BE1-9195CF4D7055 | - |
Αναγνωριστικό | https://doi.org/10.1080/15567036.2011.582600 | - |
Γλώσσα | en | - |
Μέγεθος | 9 pages | en |
Τίτλος | Hydrocarbons plays and prospectivity of the Mediterranean ridge | en |
Δημιουργός | Manoutsoglou Emmanouil | en |
Δημιουργός | Μανουτσογλου Εμμανουηλ | el |
Δημιουργός | Pantopoulos, G | en |
Δημιουργός | Makrodimitras ,G | en |
Δημιουργός | Konstantopoulos Panagiotis | en |
Δημιουργός | Κωνσταντοπουλος Παναγιωτης | el |
Εκδότης | Taylor & Francis | en |
Περίληψη | The 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 |
Τύπος | Peer-Reviewed Journal Publication | en |
Τύπος | Δημοσίευση σε Περιοδικό με Κριτές | el |
Άδεια Χρήσης | http://creativecommons.org/licenses/by/4.0/ | en |
Ημερομηνία | 2015-10-29 | - |
Ημερομηνία Δημοσίευσης | 2015 | - |
Θεματική Κατηγορία | Hydrocarbons | en |
Βιβλιογραφική Αναφορά | A. 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 |