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The importance of the Triassic-Jurassic unconformity to the hydrocarbon potential of BulgariaNormal access

Authors: G. Georgiev and A. Atanasov
Journal name: First Break
Issue: Vol 11, No 11, November 1993 pp. 489 - 497
DOI: 10.3997/1365-2397.1993025
Language: English
Info: Article, PDF ( 1.42Mb )
Price: € 30

Summary:
Bulgaria occupies 110 000 km2 of territory on the Balkan Peninsula, which includes numerous, varied tectonic units. The Balkanide Alpine belt, which is part of the Alpine-Himalayan orogenic chain, divides the territory into two parts - north and south, each with its own geological features (Figs land 2). In southern Bulgaria igneous and metamorphic rocks are widespread .. Four different orogenic units dominate (Fig. 2)-the so-called Srednogorie, Kraistide, Rhodope massifs and the Sakar-Strandja zone. Several quite smalI, shallow and discrete Palaeogene-Neogene basins are developed in these zones, but none has hydrocarbon potential.


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