Otmas (Eremenko) N.M.
huminga@yandex.ru
Graduated from Saint Petersburg State University, specialization «geomorphology, Quaternary geology and paleogeography of the polar regions» (2011).
Engineer of the Department of stratigraphy of petroleum provinces, VNIGRI.
Area of scientific interests: lithology and facies analysis, study of reservoirs.
Has 16 publications.
| Article # 27_2016 | submitted on 03/23/2016 displayed on website on 07/20/2016 |
| 14 p. | Otmas (Eremenko) N.M., Zhuravlev A.V. |
| Lithofacial features of the Lower Serpukhovian strata (Lower Carboniferous) from the south of Chernyshev Uplift and Kosyu-Rogov depression | |
| The lithological description and facial interpretation of the Lower Serpukhovian sediments from the Izyayu River (south of Chernyshev uplift) are given. The section is represented by deep-water deposits, the distribution of which is expected in the southern part of Kosyu-Rogovsky depression.
Keywords: Lower Carboniferous, Serpukhovian stage, facies, Chernyshev uplift, Kosyu-Rogovsky depression. |
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| article citation | Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny [Lithofacial features of the Lower Serpukhovian strata (Lower Carboniferous) from the south of Chernyshev Uplift and Kosyu-Rogov depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 3, available at: http://www.ngtp.ru/rub/2/27_2016.pdf |
| DOI | https://doi.org/10.17353/2070-5379/27_2016 |
Irwin M.L. General theory of epeiric clear water sedimentation. Bull. Amer. Assoc. Petrol. Geol. 49, 1965, p. 445-459.
Kossovaya O.L., Vevel Y.A., Zhuravlev A.V. Fauna and sedimentation near the Visean/Serpukhovian boundary (Izyayu River section, Tchernyshev Swell, Subpolar Urals). Newsletter on Carboniferous Stratigraphy, 2001, no. 19, p. 29-31.
Shishlov S.B. Strukturno-geneticheskiy analiz osadochnykh formatsiy [Structural and genetic analysis of sedimentary formations]. St. Petersburg: SPbGGI, 2010, 276 p.
Timonin N.I. Tektonika gryady Chernysheva (Severnoe Priural'e) [Tectonics of Chernyshev ridge (the North Urals)]. Leningrad: Nauka, 1975, 130 p.
Vevel' Ya.A., Zhuravlev A.V., Kossovaya O.L. Smena faunisticheskikh assotsiatsiy na granitse vizeyskogo i serpukhovskogo yarusov na gryade Chernysheva (Pripolyarnyy Ural) [Change of faunal associations on the boundary of Visean and Serpukhovian stage on the Chernyshev ridge (Polar Urals)]. Abstracts of XLVI session of the Paleontological Society. St. Petersburg, 2000, p. 19-20.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian - Lower Carboniferous of the north-east of European Russia]. St. Petersburg: Izd-vo VSEGEI, 2003, 85 p.
Zhuravlev A.V., Sobolev D.B. Konodonty pogranichnykh vizeysko-serpukhovskikh otlozheniy yuzhnoy chasti gryady Chernysheva (r. Iz"yayu) [Conodonts of the border Visean-Serpukhovian deposits of the southern part of the Chernyshev ridge (Izyayu River)]. Trudy IG Komi NTs UrO RAN, vol. 102. Syktyvkar, 2000, p. 84-89.
| Article # 35_2012 | submitted on 05/18/2012 displayed on website on 07/10/2012 |
| 12 p. | Otmas (Eremenko) N.M., Murav'eva Yu.A. |
| Application of the X-ray microtomography for porosity determination in borehole core | |
| The results of the porosity and permeability study of the carbonate samples came from the 1 Yun’yaha borehole are discussed. This study was carried out using traditional and tomographic methods. X-ray tomography demonstrates connection of the porosity and permeability of the studied samples with pore morphology and lithological and genetic types of sediments. Key words: microtomography, lithology, carbonates, porosity, permeability. |
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| article citation | Eremenko N.M., Murav’eva Yu.A. Primenenie metodov rentgenovskoy mikrotomografii dlya opredeleniya poristosti v kerne skvazhin [Application of the X-ray microtomography for porosity determination in borehole core]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 3, available at: http://www.ngtp.ru/rub/2/35_2012.pdf |
Arns C.H., Bauget F., Limaye A., Sakellariou A., Senden T.J., Sheppard A.P., Sok R.M., Pinczewski W.V., Bakke S., Berge L.I., Oren P.-E., and Knackstedt M.A. Pore-Scale Characterization of Carbonates Using X-Ray Microtomography. Society of Petroleum Engineers Journal, 2005, vol. 10, no. 4, pp. 475-484.
Ivanov V.V., Toropov V.A., Utkina O.L., Gudel'man A.A. Geologicheskoe stroenie Lemvinskogo poperechnogo opuskaniya po rezul'tatam geologo-razvedochnykh rabot OOO «Gazprom pererabotka» [Geological structure of the Lemvin cross subsidence based on results of exploration of LLC "Gazprom Recycling»]. Geologiya, burenie, razrabotka i ekspluatatsiya gazovykh i gazokondensatnykh mestorozhdeniy, 2010, no. 3, pp. 10-24.
Peters E.J., Afzal N. Characterization of heterogeneities in permeable media with computed tomography imaging. Journal of Petroleum Science and Engineering, 1992, no. 7, pp. 283–296.
Saadat K., Rahimpour-Bonab H., Esfahani M.R., Vali J. Empirical correlation for porosity deduction from X-ray computed tomography (CT). JGeope, 2011, 1(2), pp. 47-54.
Tafforeau P., Boistel R., Boller E., Bravin A., Brunet M., Chaimanee Y., Cloetens P., Feist M., Hoszowska J., Jaeger J.-J., Kay R.F., Lazzari V., Marivaux L., Nel A., Nemoz C., Thibault X., Vignaud P., Zabler S. Applications of X-ray synchrotron microtomography for non-destructive 3D studies of paleontological specimens. Applied Physics, 2006, a. 83, pp. 195–202.
Wellington, S.L., Vinegar, H.J. X-ray computerized tomography. Journal of Petroleum Technology 39, 1987, рр. 885–898.
Zhukova T.V. Rol' mikropaleontologicheskikh i litologo-petrograficheskikh issledovaniy pri raschlenenii i korrelyatsii raznofatsial'nykh tolshch devona i karbona v razreze skvazhiny 1-Yun'yakhinskaya [The role of micropaleontological and lithological and petrographic studies in separation and correlation of the Devonian and Carboniferous different-facial strata in borehole 1 Yun’yaha]. Proceedings of the All-Russian Lithological Meeting “Rify i karbonatnye psefitolity” [Reefs and carbonate psephitolits]. Syktyvkar: Geoprint, 2010, pp. 64-66.
Zhuravlev A.V., Vevel’ Ya.A. Vozmozhnosti ispol'zovaniya vychislitel'noy mikrotomografii v mikropaleontologicheskikh i litologicheskikh issledovaniyakh [Possibilities of computed microtomography application in micropalaeontological and lithological studies]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 2, available at: http://www.ngtp.ru/rub/2/21_2012.eng.pdf
| Article # 45_2009 | submitted on 12/10/2009 displayed on website on 12/14/2009 |
| 20 p. | Otmas (Eremenko) N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. |
| Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches | |
| The results of complex studying the Upper Devonian - Lower Carboniferous key sequence on the Talota river (north of the Vashutkino-Talota zone of overthrusts, Timan-Pechora province) are presented. The tectonic twinning of the sequence on the zone of overthrusts is proved by biostratigraphy data. The parautochthonous and allochthonous parts of the sequence are dated by foraminifera and conodonts. The first part contains Early Famenian-Late Visean deposits, the second part - Late Famenian-Serpukhovsk deposits. Breaks in sedimentations are established in the Lower Tournaisian and Lower Visean. The presence of an ancient secondary prefolded component of magnetization, confined to the definite parts of the sequence and caused by tectonic and hypergene processes, is established. The direction of this magnetization allowed reconstructing the prefolded (Middle Paleozoic) position of the allochthone and parautochthone. Key words: Upper Devonian, Lower Carboniferous, key sequence, Timan-Pechora province, stratigraphy, paleomagnetology, tectonics. Sequence description by Eremenko N.M. and Zhuravlev A.V. is provided in the Annex 1. |
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| article citation | Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches // Neftegazovaya Geologiya. Teoriya I Praktika. - 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/45_2009.pdf Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches // Neftegazovaya Geologiya. Teoriya I Praktika. - 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/45prilojenie_2009.pdf |
| Article # 39_2009 | submitted on 11/06/2009 displayed on website on 11/30/2009 |
| 9 p. | Zhuravlev A.V., Otmas (Eremenko) N.M. |
| Peculiarities of structure and the conditions of forming the Lower-Middle Devonian Padeya formation, Central Pay-Khoy | |
| Description of the sequences of the Lower-Middle Devonian Padeya formation in Central Pay-Khoy is given. The conditions of forming this formation are restored on the basis of texture and structure characteristics of the deposits: mainly a turbidite nature of formation cyclites is suggested. A seismic reflector III1 is apparently due to the unit of the sandy-mudstone gradation cyclites in the formation upper part. Key words: Padeya formation, Lower Devonian, Middle Devonian, Central Pay Khoy. |
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| article citation | Zhuravlev A.V., Eremenko N.M. Peculiarities of structure and the conditions of forming the Lower-Middle Devonian Padeya formation, Central Pay-Khoy // Neftegazovaya Geologiya. Teoriya I Praktika. – 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/39_2009.pdf |
| Article # 9_2009 | submitted on 03/12/2009 displayed on website on 03/18/2009 |
| 11 p. | Otmas (Eremenko) N.M. |
| Detailed sedimentological characteristics of the lower Moscovian deposits in the borehole Anyb 3-R (North-Keltma structure of the Cis-Timanian depression) | |
| Three transgressive-regressive cycles are established in the Lower Moscovian interval (Middle Carboniferous) on the data of Anyb well core sedimentological analysis. These cycles with taking into consideration biostratigraphical data have been correlated with the Staromonetny (Vereian horizon), Yambirny and Tsninsky (Kashirian horizon lower part) cycles in the Moscow syneclise type sections. Key words: Severokiltminskaya structure, Middle Carboniferous, sedimentological analysis, biostratigraphy, foraminifers, conodonts. |
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| article citation | Eremenko N.M. Detailed sedimentological characteristics of the lower Moscovian deposits in the borehole Anyb 3-R (North-Keltma structure of the Cis-Timanian depression) // Neftegazovaya Geologiya. Teoriya I Praktika. – 2009. - V.4. - #1.- http://www.ngtp.ru/rub/2/9_2009.pdf |