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Geology of the Strait of Sicily: An example of geological mapping

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:5749031
The Strait of Sicily is a comparatively shallow-water threshold which divides the Mediterranean into western and eastern deep-water hollows. The author composed a geologic map of the bottom of the Sicilian Strait and adjacent aquatories with a scale of 1:500,000. This map is based on the geologic-geophysical data of Soviet and foreign investigations (including more than 15,000 km of seismic reflection profiles, dredging, sampling, and drilling data) and their seismostratigraphic interpretation. Most of this region is underlain by the continental crust with a thick sedimentary cover. The most widespread sediments are Pliocene-Quaternary. On the map they are shown only in basins where thickness exceeds 200 m (Hammamet, Gabes, Tunisian, etc). Additionally, there are mapped outcrops of Messinian evaporites at the steep slopes of the Malta escarpment, Pantelleria and Malta grabens, Adventure and Skerki banks, etc. Also shown are outcrops of Paleogene, Cretaceous, Jurassic, and Upper Triassic rocks. This new geologic map should generate great interest because of the high petroleum potential of this region.
OSTI ID:
5749031
Report Number(s):
CONF-8809346--
Conference Information:
Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (USA) Journal Volume: 72:8
Country of Publication:
United States
Language:
English

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