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Tectonically, Montenegro lies in a zone between the Dinarides and the Hellenides which are the southern branch of the Alps extending south along the East coast of the Adriatic and Ionian Seas.

Onshore the zone comprises southwest facing folds and thrusts formed during the Miocene and Early Pliocene. Most of onshore Montenegro is mountainous and has an uplifted, eroded and highly faulted sedimentary cover. Globalshift believes it is unlikely that any potential oil and gas resources could have survived this recent geological history.

Offshore the Dinarides fold belt is separated from the Italian Apennine fold belt by the Adriatic foredeep basin. The stratigraphy is dominated by a Mesozoic to Middle Eocene rift to passive margin sequence with a significant thickness of platform carbonates, shales and evaporites with a number of potential source, reservoir and seal intervals.

Palaeogene and Neogene turbidite shales and sandstones form the foredeep sequence in front of and beneath the carbonate thrusts. Structures could contain biogenic gas in Pliocene and Pleistocene traps within the foredeep basin in a similar fashion to many of the Italian and Croatian offshore gas fields.

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