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- W1521724231 abstract "in the Timan-Pechora province. Practically all the proved reserves are in the Lower Permian-Carboniferous complex. It is at dep ths of 1500-2500 m. The lower Frasnian-Middle Devonian complex, which contains pools of light oil in many areas, is at a depth of 4000-5000 m and has been studied less. The main zone of development of the lower Frasnian-Middle Devonian complex is the Pechlora-Kolvin oil-gas area (aulacogen), which includes the Kolvin mega-arch. The greatest thicknesses of these sediments here are in depressions of the basement. The largest of these is the Khar’yagin. Their thickness here is 413 m in one well. In the Layavozh basement depression seismic surveys indicate that the Middle Devonian is more than 400 m thick. The Middle Devonian is absent, however, at the crests of the baseme nt highs. See Fig. 1 for location of structures. Pashiy clastic sediments (Frasnian stage in lower part of Upper Devonian) are more widely distributed in the north of the province than are the Middle Devonian sediments; they occur from the Malozemel’sko Kolguyev monocline on the west to the Sorokina arch on the east. The Pashiy deposits rest transgressively on rocks from Ordovician to Middle Devonian in age. In comparison with the Middle Devonian sediments, the Pashiy sandstones are not as persistent and are commonly not good reservoirs." @default.
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- W1521724231 date "1981-01-01" @default.
- W1521724231 modified "2023-09-28" @default.
- W1521724231 title "Prospects for Exploration for Oil and Gas Pools in the Lower Frasnian-Middle Devonian Oil-Gas Complex in the Northern Regions of the Timan-Pechora Province" @default.
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