Specialist in lithology, sedimentology, stratigraphy, in Late Paleozoic deposits.
Professor of St. Petersburg State Mining University.
PhD in geology and mineralogy.
Research interests: lithology, stratigraphy, regional geology.
Scientific activities: development of methodology for structural and genetic analysis of sedimentary formations, making local and regional stratigraphic schemes, geological mapping and coal potential forecast of Taimyr. Author of about 70 scientific papers.
|Article # 19_2012||submitted on 02/29/2012 displayed on website on 04/19/2012|
|24 p.||Shishlov S.B., Gubaeva F.R.|
|Structure and formation conditions of the Lower Cretaceous reservoir BV-8 - Povkhovskoe oil field (Western Siberia)|
|Structural and genetic analysis of cores and log data (SP curves) has shown that strata BV-8 of the Povkhovskoe oil field consists of 10 transgressive-regressive systems of layers, which were formed as a result of migration landscapes (deep muds, “rag sands” and sand dikes) during the rise and fall of the sea level. It has been found that sand strata are represented by lenses that consist of two layers: the lower (accumulated in the final phase of regression), and the upper (accumulated at the beginning of transgression of the next sedimentation cycle). The obtained results do not confirm the clinoform model of strata BV-8 due to low resolution of seismic profiling, which only allows to reveal some general boundaries of a number of diachronic sands lenses, that are located en echelon and overlap each other.
Key words: sedimentary environments, transgressive-regressive cycles, structural and genetic analysis, clinoform, productive strata BV-8, Povkhovskoe oil field, Lower Cretaceous.
|article citation||Shishlov S.B., Gubaeva F.R. Stroenie i usloviya formirovaniya rannemelovogo produktivnogo plasta BV-8 Povkhovskogo neftyanogo mestorozhdeniya (Zapadnaya Sibir') [Structure and formation conditions of the Lower Cretaceous reservoir BV-8 - Povkhovskoe oil field (Western Siberia)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 2, available at: http://www.ngtp.ru/rub/2/19_2012.pdf|
Zhuravlev E.G., Zhuravleva L.M. Osobennosti poiskov zalezhey v achimovskoy tolshche Zapadnoy Sibiri [Features of deposit prospecting in Western Siberia Achimov strata]. XIX Gubkinskie chteniya. Moscow: RGU nefti i gaza, 2011, pp. 29-30.
|Article # 16_2011||submitted on 04/06/2011 displayed on website on 04/27/2011|
|18 p.||Zherlygin A.L., Shishlov S.B., Zhuravlev A.V., Vevel Ya.A.|
|Structure and genesis history of Kara-Silovoyahsky devonian organogenic complex (southeastern Pai-Khoi)|
|New data about the size, shape, composition and structural features of the Devonian organogenic complex (Kara Silova-Yakha interfluve, southeastern Pai-Khoi) are presented. The interpretation of these features is related together with reconstruction of genesis history of this organogenic complex, under the influence of the transgressive-regressive phases of the paleobasin evolution. The study results can be used in geological mapping and in core analysis of wells of the Pre-Urals Trough, where prospective hydrocarbon reservoirs are related to the brecciated aprons, produced by crushing and fracturing of such organogenic structures.
Key words: Pai-Khoi, the Devonian period, conodonts, organogenic complex, lithotypes, genesis history, morpho-litho-stratigraphic unit.
|article citation||Zherlygin A.L., Shishlov S.B., Zhuravlev A.V., Vevel Ya.A. Stroenie i istoriya formirovaniya Kara-Silovoyakhskogo devonskogo organogennogo massiva (yugo-vostochnyy Pay-Khoy) [Structure and genesis history of Kara-Silovoyahsky devonian organogenic complex (southeastern Pai-Khoi)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 2, available at: http://www.ngtp.ru/rub/2/16_2011.pdf|
|Article # 3_2008||displayed on website on 01/16/2008|
|24 p.||Shishlov S.B.|
|Sequence stratigraphy of the Upper Paleozoic, Kolguev Island|
|The developed and published lithological-genetic typification of Kolguev Island Upper Paleozoic deposits allowed generalizing the materials received by interval core recovery from a series of exploration wells. The basic regularities in localization of established lithotypes have been determined on the basis of constructing a series of lithological-genetic profiles. As a result six sequences - natural historical geological bodies - have been established. Their forming is associated with the large transgressive-regressive cycles of sedimentation. More complete idea of the peculiarities of structure of the Kolguev Island Upper Paleozoic is received.
Key words: Kolguev Island, Upper Paleozoic, transgressive-regressive cycles of sedimentation, sequence stratigraphy
|article citation||Shishlov S.B. Sequence stratigraphy of the Upper Paleozoic, Kolguev Island // Neftegazovaya Geologiya. Teoriya I Praktika. – 2008. - V.3. - #1.- http://www.ngtp.ru/rub/2/3_2008.pdf|