The Ionian zone is the main object of seismic interpretation for a long time. Within this framework, we shall analyze the new seismic intrpretation methods used in oil and gas exploration in the western part of Ionian zone. The Ionian zone is very complex involving certain tectonic faults. In the central part, we can see the duplex tectonic style. Anticline belts from east to west can be interpreted.The Ionian zone comprises three anticline belts:Berati belt, Kurveleshi belt and Cika belt. By application of SeisWork2D in the eastern part of the belt, we have evidenced some perscpective structures, meanwhile in the western part, the seismic quality is very chaotic. Kurveleshi belt is constructed by structures of various forms and dimensions ...
Seismicity in the Ionian Sea (W. Greece) is mainly generated along the Cephalonia–Lefkada Transform ...
Summarization: Contractional structures recognised in a recent SW-NE oriented seismic profile offsho...
We analyzed the structure and evolution of the external Calabrian Arc (CA) subduction complex throug...
The study area is located in the sourthen part of Albania. The paper presents the geological – geoph...
AbstractThe external thrustbelt of Albania consists of some tectonic zones (Ionian, Kruja and Krasta...
The Ionian and Gavrovo Zones in the external Hellenide fold-and-thrust belt of western Greece are a ...
The area under studying is situated in the western part of Albania. A number of oilfields within the...
The Ionian and Gavrovo Zones in the external Hellenide fold-and-thrust belt of western Greece are a ...
The Kruja zone and the Ionian one are integral parts of the Albanian Thrust Belt, which lie directly...
Although Albania constitutes a relatively small country, it displays a unique petroliferous foreland...
The presented crustal section under the Ionian Sea is the result of refractional seismic work on two...
Albania belongs to the Dinaric-Albanid-Hellenides arch of alpine orogeny. There are four main geolog...
The interpretation of the CROP-MARE deep seismic lines has revealed the structure of the Ionian crus...
In western Greece, the Ionian and pre-Apulian zones represent, respectively, the basin and the trans...
The Miocene to Recent tectonic evolution of the Cilicia Basin near the present day mouth of the Goks...
Seismicity in the Ionian Sea (W. Greece) is mainly generated along the Cephalonia–Lefkada Transform ...
Summarization: Contractional structures recognised in a recent SW-NE oriented seismic profile offsho...
We analyzed the structure and evolution of the external Calabrian Arc (CA) subduction complex throug...
The study area is located in the sourthen part of Albania. The paper presents the geological – geoph...
AbstractThe external thrustbelt of Albania consists of some tectonic zones (Ionian, Kruja and Krasta...
The Ionian and Gavrovo Zones in the external Hellenide fold-and-thrust belt of western Greece are a ...
The area under studying is situated in the western part of Albania. A number of oilfields within the...
The Ionian and Gavrovo Zones in the external Hellenide fold-and-thrust belt of western Greece are a ...
The Kruja zone and the Ionian one are integral parts of the Albanian Thrust Belt, which lie directly...
Although Albania constitutes a relatively small country, it displays a unique petroliferous foreland...
The presented crustal section under the Ionian Sea is the result of refractional seismic work on two...
Albania belongs to the Dinaric-Albanid-Hellenides arch of alpine orogeny. There are four main geolog...
The interpretation of the CROP-MARE deep seismic lines has revealed the structure of the Ionian crus...
In western Greece, the Ionian and pre-Apulian zones represent, respectively, the basin and the trans...
The Miocene to Recent tectonic evolution of the Cilicia Basin near the present day mouth of the Goks...
Seismicity in the Ionian Sea (W. Greece) is mainly generated along the Cephalonia–Lefkada Transform ...
Summarization: Contractional structures recognised in a recent SW-NE oriented seismic profile offsho...
We analyzed the structure and evolution of the external Calabrian Arc (CA) subduction complex throug...