The Epsilon field, is located at the centre of Prinos oil basin (N. Aegean, Greece), 11 km NW of the island of Thassos and 4 km NW of the Prinos field, the first productive oil field in the Aegean Sea. The taphrogenetic basin of Prinos has been widely studied, due to its hydrocarbon reservoirs. Extensive geophysical survey, started at early 1970 ‘s, led to a number of drilling jobs, which confirmed the existence of hydrocarbons in the area. The combined geological information, derived from the analysis of lithological, stratigraphic and geochemical data of the basin, suggested a structural and depositional model, strongly related to the Miocene tectonics and sedimentation. The new geophysical and drilling data from Epsilon oil field, are co...
Summarization: Fifty-one mudstone samples were collected from the Miocene successions in Lefkas and ...
SUMMARY. — The Tuz Gölü basin is a NW-SE trending intramontane basin situated in a transverse struct...
The studied area is a 130 km long fast spreading graben in Central Greece. Its complex geodynamical ...
An extentional tectonic led to the formation of the basin along marginal listric faults. The fast su...
Summarization: This work presents the results of an extended geochemical study, aiming to identify t...
Summarization: Conditions favoring generation, migration and trapping of hydrocarbons generated econ...
Abstract: Cored samples from four wells from Prinos, Prinos North and Epsilon fields have been analy...
An extentional tectonic led to the formation of the basin along marginal listric faults. The fast su...
In western Greece, the Ionian and pre-Apulian zones represent, respectively, the basin and the trans...
Summarization: Results of the current and already published studies suggest that the Tortonian in ag...
The Ionian and Gavrovo Zones in the external Hellenide fold-and-thrust belt of western Greece are a ...
The Ionian and Gavrovo Zones in the external Hellenide fold-and-thrust belt of western Greece are a ...
Results of the current and already published studies suggest that the Tortonian in age deposits coul...
The Akropotamos area constitutes a new geothermal field located in the eastern coastal zone of the S...
The sedimentary sequence of the south Thrace Basin (northwest Turkey) comprises Upper Cretaceous-Hol...
Summarization: Fifty-one mudstone samples were collected from the Miocene successions in Lefkas and ...
SUMMARY. — The Tuz Gölü basin is a NW-SE trending intramontane basin situated in a transverse struct...
The studied area is a 130 km long fast spreading graben in Central Greece. Its complex geodynamical ...
An extentional tectonic led to the formation of the basin along marginal listric faults. The fast su...
Summarization: This work presents the results of an extended geochemical study, aiming to identify t...
Summarization: Conditions favoring generation, migration and trapping of hydrocarbons generated econ...
Abstract: Cored samples from four wells from Prinos, Prinos North and Epsilon fields have been analy...
An extentional tectonic led to the formation of the basin along marginal listric faults. The fast su...
In western Greece, the Ionian and pre-Apulian zones represent, respectively, the basin and the trans...
Summarization: Results of the current and already published studies suggest that the Tortonian in ag...
The Ionian and Gavrovo Zones in the external Hellenide fold-and-thrust belt of western Greece are a ...
The Ionian and Gavrovo Zones in the external Hellenide fold-and-thrust belt of western Greece are a ...
Results of the current and already published studies suggest that the Tortonian in age deposits coul...
The Akropotamos area constitutes a new geothermal field located in the eastern coastal zone of the S...
The sedimentary sequence of the south Thrace Basin (northwest Turkey) comprises Upper Cretaceous-Hol...
Summarization: Fifty-one mudstone samples were collected from the Miocene successions in Lefkas and ...
SUMMARY. — The Tuz Gölü basin is a NW-SE trending intramontane basin situated in a transverse struct...
The studied area is a 130 km long fast spreading graben in Central Greece. Its complex geodynamical ...