Трудноизвлекаемые запасы, нетрадиционные источники углеводородного сырья
Ответственный за рубрику – доктор геолого-минералогических наук А.В. Петухов
| Статья № 10_2018 | дата поступления в редакцию 12.03.2018 подписано в печать 30.03.2018 |
| 25 с. | Морариу Д., Аверьянова О.Ю. |
| Образование кливажа пелитовых пород в диагенезе-начале катагенеза - важный фактор создания путей миграции углеводородов *Статья представлена на английском языке
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| Литификация пелитовых пород, обладающих углеводородным потенциалом, на стадии диагенеза, и дальнейшее их уплотнение на стадии катагенеза приводят к сокращению пористости-проницаемости, закрытию путей миграции флюидов и возможному «перегреву» органического вещества. В определенных тектонических условиях развитие вторичной структуры осадочных пород в виде густой сети трещин первичного и вторичного кливажа может создавать достаточные объемы пространства с расстояниями между слоями сланцеватости, варьирующими от 20 до 150 мкм, которые в свою очередь могут представлять собой пути миграции флюидов и углеводородов. Участки с развитием пород, обладающих благоприятным петрогенным профилем (пелитовые породы со сложной сланцеватостью при устойчивых температурах, не превышающих 100-150°С), могут рассматриваться как потенциальные пути миграции углеводородов.
Изучение участков пород, потенциальный миграционный потенциал которых резко уменьшается с повышением температуры во время погружения и затем частично компенсируется образованием кливажа, может представлять собой определённый интерес для оценки потенциала и перспектив нефтегазоносности.
Ключевые слова: пелитовая порода, расстояние между слоями сланцеватости, первичный и вторичный кливаж, пути миграции углеводородов, нефтегазоносность. |
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| ссылка на статью обязательна | Morariu D., Averyanova O.Yu. Сleavage fabric – significant faсtor creating discrete hydrocarbon migration pathways in diagenetic to low metamorphic pelites // Нефтегазовая геология. Теория и практика. – 2018. - Т.13. - №1. - http://www.ngtp.ru/rub/9/10_2018.pdf |
| цифровой идентификатор статьи DOI | https://doi.org/10.17353/2070-5379/10_2018 |
Литература
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Chalmers G., R.M. Bustin and I. Powers, 2009. A pore by any other name would be as small: The importance of meso- and microporosity in shale gas capacity (abs.): AAPG Search and Discovery article 90090, 1 p.: http://www.searchanddiscovery.com/abstracts/html/2009/annual/abstracts/chalmers.htm (accessed March 14, 2011).
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Glasmacher U.A, Bauer W., Clauer N., Puchkov V.N., 2004. Neoproterozoic metamorpishm and deformation at the southeastern margin of the East European Craton Uralides, Russia. International Journal of Earth Sciences (Geol Rundsch) (2004) November 2004, Volume 93, Issue 5, pp. 921–944. DOI: https://doi.org/10.1007/s00531-004-0426-3
Jacob G., H.J. Kisch, and B.A. van der Pluijm, 2000. The relationship of phyllosilicate orientation, X-ray diffraction intensity ratios, and c/b fissility ratios of the Helvetic zone of the Swiss Alps and the Caledonides of Jamtland, central western Sweden: Journal of Structural Geology, 22 (2), p. 245-258.
Katsube T.J., 2000. Shale permeability and pore-structure evolution characteristics, Geological Survey of Canada. Report 2000, E15, 9 p.
Katsube T.J., M.A. Williamson, 1998. Shale petrophysical characteristics: permeability history of subsiding shales; in Shales and Mudstones II: Petrography, Petrophysics, Geochemistry and Economic Geology, (ed.) J. Schieber, W. Zimmerle, and P.S. Sethi; E. Schweizerbart Science Publishers, Stuttgart, Germany, p. 69-91.
Kisch H.J., 1990. Calibration of the anchizone: a critical comparison of illite ‘crystallinity’ scales used for definition, Journal of Metamorphic Geology, 8: 31–46. DOI: https://doi.org/10.1111/j.1525-1314.1990.tb00455.x
Kisch, H.J., 1991. Development of slaty cleavage and degree of very low grade metamorphism: a review. Journal of Metamorphic Geology, 9, pp. 735–750. DOI: https://doi.org/10.1111/j.1525-1314.1991.tb00562.x
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Loucks R.G., M.R. Reed, S.C. Ruppel and U. Hammes, 2012. Spectrum of pore types and networks in mudrocks and a descriptive classification for matrix-related mudrock pores, AAPG Bulletin, v. 96, no. 6 (June 2012), pp. 1071–1098. DOI: https://doi.org/10.1306/08171111061
Mastalerz, M., A. Schimmelmann, A. Drobniak, and Y. Chen, 2013, Porosity of Devonian and Mississippian New Albany Shale across a maturation gradient: Insights from organic petrology, gas adsorption, and mercury intrusion, AAPG Bulletin, v. 97, no. 10 (October 2013), pp. 1621–1643. DOI: https://doi.org/10.1306/04011312194
Merriman, R.J., Peacor, D.R., 1999. Very low-grade metapelites: mineralogy, microfabrics and measuring reaction progress. In: Frey, M., Robinson, D. (Eds.), Low-grade metamorphism. Blackwell Science, Oxford, pp. 10–60.
Microstructure of fine-grained sediments: from mud to shale, 1991. Editors: Bennett, R.H., Bryant, W.R., Hulbert, M.H., Associated Editors: Chiou, W.A., Faas, R.W., Kasprowicz, J., Li, H., Lomenick, T., O`Brien, N.R., Pamukcu, S., Smart, P., Weaver, C.E., Yamamoto, T. Springer New York. 1991, 566 p. DOI: https://doi.org/10.1007/978-1-4612-4428-8
Mondol, N.H., K. Bjorlykke, J. Jahren, and K. Hoeg, 2007, Experimental mechanical compaction of clay mineral aggregates - changes in physical properties of mudstones during burial: Marine and Petroleum Geology, v. 24, p. 289–311. DOI: https://doi.org/10.1016/j.marpetgeo.2007.03.006
Nelson, H.P., 2009. Pore throat sizes in sandstones, tight sandstones and shale: AAPG, V. 93, no 3, 329-340 p. DOI: https://doi.org/10.1306/10240808059
Neuzel, C.E., 1994, How permeable are clays and shales? Water Resources Research, vol. 30, no. 2 (February 1994), p. 145-150.
Park A.F., 2009. Cleavages developed in mudstone during diagenesis and deformation: an example from the Carboniferous (Tournaisian), southeastern New Brunswick, Canada: Atlantic Geology 45 (2009), pp. 204–216. DOI: https://doi.org/10.4138/atlgeol.2009.010
Passchier, C.W., Trouw, R.A.J., 2005. Microtectonics. Springer-Verlag Berlin Heidelberg, 366 p. DOI: https://doi.org/10.1007/3-540-29359-0
Rouquerol, J., D. Avnir, C.W. Fairbridge, D.H. Everett, J.H. Haynes, N. Pernicone, J.D. F. Sing and K.K. Unger, 1994. Recommendations for the characterization of porous solids: Pure and Applied Chemistry, v. 66, p. 1739–1758. DOI: https://doi.org/10.1351/pac199466081739
Rushing, J.A., 2014. Petrophysics of Shale Reservoirs: Understanding the rocks, pores, fluids and their interactions. AMU PETE 631 Lecture College Station, TX (USA) - 07 April 2014. 102 p. http://www.pe.tamu.edu/blasingame/data/z_zCourse_Archive/P631_14A/P631_14A_Lectures/P631_14A_Lec_xx_...
Schieber, J., 2011. Shale microfabrics and pore development - An overview with emphasis on the importance of depositional processes, Recovery – 2011 CSPG CSEG CWLS Convention, 4 p.
Schmoker J.W., 1995. Method for assessing continuous-type (unconventional) hydrocarbon accumulations, in Gautier D.L., Dolton G.L., Takahashi K.I, and Varens K.L., eds., 1995, 1995 National assessment of United States oil and gas resources – Results, methodology, and supporting data: U.S. Geological Survey Bulletin Data Series DDS-30, 1 CD-ROM.
Syed A.A., Clark W.J., Moore W.R., Dribus J.R., 2010. Diagenesis and reservoir quality // Oilfield Review Summer 2010:22, no.2. – 14-27 p. https://www.slb.com/~/media/Files/resources/oilfield_review/ors10/sum10/composite.pdf
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Van der Pluijm, B.A. & Kaars-Sijpesteijn, C.H., 1983. Chlorite-mica aggregates: morphology, orientation, development and bearing on cleavage formation in very low-grade rocks. Journal of Structural Geology, V.6, pp. 399-407.
Van Sickel, W.A., Kominz, M.A., Miller, K.G., & Browning, J.V. (2004). Late Cretaceous and Cenozoic sea-level estimates: Backstripping analysis of borehole data, onshore New Jersey. Basin Research, 16(4), 451-465. DOI: https://doi.org/10.1111/j.1365-2117.2004.00242.x
Vazquez M., L. Asebriy, A. Azdimousa, A. Jabaloy, G. Booth-Rea, L. Barbero, M. Mellini, F. Gonzalez-Lodeiro, 2013. Evidence of extensional metamorphism associated to Cretaceous rifting of the North-Maghrebian massive margin: The Tanger-Ketama Unit (External Rif, northern Morocco): Geologica Acta, Vol. 11, N3, September 2013, pp. 277-293. DOI: https://doi.org/10.1344/105.000001843
Weaver C.E., 1984. Shale-Slate Metamorphism in Southern Appalachians Developments in Petrology. V. 10, 239 p.
Winkler, H.G.F., 1974. Petrogenesis of Metamorphic Rocks. English editor E. Froese. Springer Study Edition, 3rd edition, Springer-Verlag, Berlin, Heidelberg, New York. 320 p.
Bridge J.S., and R.V. Demicco, 2008, Earth surface processes, landforms and sediment deposits: New York, Cambridge University Press, 830 p.
Bucher K. and M. Frey, 2002. Petrogenesis of Metamorphic Rocks. Springer-Verlag; Berlin, Heidelberg; pp. 341.
Chalmers G., R.M. Bustin and I. Powers, 2009. A pore by any other name would be as small: The importance of meso- and microporosity in shale gas capacity (abs.): AAPG Search and Discovery article 90090, 1 p.: http://www.searchanddiscovery.com/abstracts/html/2009/annual/abstracts/chalmers.htm (accessed March 14, 2011).
Day-Stirrat, R.J., A. McDonnell, and L.J. Wood, 2010, Diagenetic and seismic concerns associated with interpretation of deeply buried “mobile schales”, in L. Wood, ed., Schale tectonics: AAPG Memoir 93, p. 5-27.
Glasmacher U.A, Bauer W., Clauer N., Puchkov V.N., 2004. Neoproterozoic metamorpishm and deformation at the southeastern margin of the East European Craton Uralides, Russia. International Journal of Earth Sciences (Geol Rundsch) (2004) November 2004, Volume 93, Issue 5, pp. 921–944. DOI: https://doi.org/10.1007/s00531-004-0426-3
Jacob G., H.J. Kisch, and B.A. van der Pluijm, 2000. The relationship of phyllosilicate orientation, X-ray diffraction intensity ratios, and c/b fissility ratios of the Helvetic zone of the Swiss Alps and the Caledonides of Jamtland, central western Sweden: Journal of Structural Geology, 22 (2), p. 245-258.
Katsube T.J., 2000. Shale permeability and pore-structure evolution characteristics, Geological Survey of Canada. Report 2000, E15, 9 p.
Katsube T.J., M.A. Williamson, 1998. Shale petrophysical characteristics: permeability history of subsiding shales; in Shales and Mudstones II: Petrography, Petrophysics, Geochemistry and Economic Geology, (ed.) J. Schieber, W. Zimmerle, and P.S. Sethi; E. Schweizerbart Science Publishers, Stuttgart, Germany, p. 69-91.
Kisch H.J., 1990. Calibration of the anchizone: a critical comparison of illite ‘crystallinity’ scales used for definition, Journal of Metamorphic Geology, 8: 31–46. DOI: https://doi.org/10.1111/j.1525-1314.1990.tb00455.x
Kisch, H.J., 1991. Development of slaty cleavage and degree of very low grade metamorphism: a review. Journal of Metamorphic Geology, 9, pp. 735–750. DOI: https://doi.org/10.1111/j.1525-1314.1991.tb00562.x
Kubler B., 1967. La cristallinite de l'illite et les zones tout a fait superieures du metamorphisme, in: Colloque sur les etages tectoniques, 1966, Neuchatel, Ed. La Braconniere, 105-122.
Loucks R.G., M.R. Reed, S.C. Ruppel and U. Hammes, 2012. Spectrum of pore types and networks in mudrocks and a descriptive classification for matrix-related mudrock pores, AAPG Bulletin, v. 96, no. 6 (June 2012), pp. 1071–1098. DOI: https://doi.org/10.1306/08171111061
Mastalerz, M., A. Schimmelmann, A. Drobniak, and Y. Chen, 2013, Porosity of Devonian and Mississippian New Albany Shale across a maturation gradient: Insights from organic petrology, gas adsorption, and mercury intrusion, AAPG Bulletin, v. 97, no. 10 (October 2013), pp. 1621–1643. DOI: https://doi.org/10.1306/04011312194
Merriman, R.J., Peacor, D.R., 1999. Very low-grade metapelites: mineralogy, microfabrics and measuring reaction progress. In: Frey, M., Robinson, D. (Eds.), Low-grade metamorphism. Blackwell Science, Oxford, pp. 10–60.
Microstructure of fine-grained sediments: from mud to shale, 1991. Editors: Bennett, R.H., Bryant, W.R., Hulbert, M.H., Associated Editors: Chiou, W.A., Faas, R.W., Kasprowicz, J., Li, H., Lomenick, T., O`Brien, N.R., Pamukcu, S., Smart, P., Weaver, C.E., Yamamoto, T. Springer New York. 1991, 566 p. DOI: https://doi.org/10.1007/978-1-4612-4428-8
Mondol, N.H., K. Bjorlykke, J. Jahren, and K. Hoeg, 2007, Experimental mechanical compaction of clay mineral aggregates - changes in physical properties of mudstones during burial: Marine and Petroleum Geology, v. 24, p. 289–311. DOI: https://doi.org/10.1016/j.marpetgeo.2007.03.006
Nelson, H.P., 2009. Pore throat sizes in sandstones, tight sandstones and shale: AAPG, V. 93, no 3, 329-340 p. DOI: https://doi.org/10.1306/10240808059
Neuzel, C.E., 1994, How permeable are clays and shales? Water Resources Research, vol. 30, no. 2 (February 1994), p. 145-150.
Park A.F., 2009. Cleavages developed in mudstone during diagenesis and deformation: an example from the Carboniferous (Tournaisian), southeastern New Brunswick, Canada: Atlantic Geology 45 (2009), pp. 204–216. DOI: https://doi.org/10.4138/atlgeol.2009.010
Passchier, C.W., Trouw, R.A.J., 2005. Microtectonics. Springer-Verlag Berlin Heidelberg, 366 p. DOI: https://doi.org/10.1007/3-540-29359-0
Rouquerol, J., D. Avnir, C.W. Fairbridge, D.H. Everett, J.H. Haynes, N. Pernicone, J.D. F. Sing and K.K. Unger, 1994. Recommendations for the characterization of porous solids: Pure and Applied Chemistry, v. 66, p. 1739–1758. DOI: https://doi.org/10.1351/pac199466081739
Rushing, J.A., 2014. Petrophysics of Shale Reservoirs: Understanding the rocks, pores, fluids and their interactions. AMU PETE 631 Lecture College Station, TX (USA) - 07 April 2014. 102 p. http://www.pe.tamu.edu/blasingame/data/z_zCourse_Archive/P631_14A/P631_14A_Lectures/P631_14A_Lec_xx_...
Schieber, J., 2011. Shale microfabrics and pore development - An overview with emphasis on the importance of depositional processes, Recovery – 2011 CSPG CSEG CWLS Convention, 4 p.
Schmoker J.W., 1995. Method for assessing continuous-type (unconventional) hydrocarbon accumulations, in Gautier D.L., Dolton G.L., Takahashi K.I, and Varens K.L., eds., 1995, 1995 National assessment of United States oil and gas resources – Results, methodology, and supporting data: U.S. Geological Survey Bulletin Data Series DDS-30, 1 CD-ROM.
Syed A.A., Clark W.J., Moore W.R., Dribus J.R., 2010. Diagenesis and reservoir quality // Oilfield Review Summer 2010:22, no.2. – 14-27 p. https://www.slb.com/~/media/Files/resources/oilfield_review/ors10/sum10/composite.pdf
TXCO Resources, 2009, The emerging resource company, TXCO Resources: Howard Weil 37th Annual Energy Conference, New Orleans, March 22–29, 2009, 35. http://www.scribd.com/doc/20128412/The-Emerging-Resource-Company (accessed March 25, 2011)
Van der Pluijm, B.A. & Kaars-Sijpesteijn, C.H., 1983. Chlorite-mica aggregates: morphology, orientation, development and bearing on cleavage formation in very low-grade rocks. Journal of Structural Geology, V.6, pp. 399-407.
Van Sickel, W.A., Kominz, M.A., Miller, K.G., & Browning, J.V. (2004). Late Cretaceous and Cenozoic sea-level estimates: Backstripping analysis of borehole data, onshore New Jersey. Basin Research, 16(4), 451-465. DOI: https://doi.org/10.1111/j.1365-2117.2004.00242.x
Vazquez M., L. Asebriy, A. Azdimousa, A. Jabaloy, G. Booth-Rea, L. Barbero, M. Mellini, F. Gonzalez-Lodeiro, 2013. Evidence of extensional metamorphism associated to Cretaceous rifting of the North-Maghrebian massive margin: The Tanger-Ketama Unit (External Rif, northern Morocco): Geologica Acta, Vol. 11, N3, September 2013, pp. 277-293. DOI: https://doi.org/10.1344/105.000001843
Weaver C.E., 1984. Shale-Slate Metamorphism in Southern Appalachians Developments in Petrology. V. 10, 239 p.
Winkler, H.G.F., 1974. Petrogenesis of Metamorphic Rocks. English editor E. Froese. Springer Study Edition, 3rd edition, Springer-Verlag, Berlin, Heidelberg, New York. 320 p.