Page 224 - Fundamentals of Gas Shale Reservoirs

204 ROCK PHYSICS ANALYSIS OF SHALE RESERVOIRS

Draege A, Jakobsen M, Johansen TA. Rock physics modelling Makarynska D, Gurevich B, Behura J, Batzle M. Fluid substitution
of shale diagenesis. Petrol Geosci 2006;12 (1):49–57. in rocks saturated with viscoelastic fluids. Geophysics 2010;75
EIA. Annual energy outlook. Washington DC: Energy Information (2):E115–E122. DOI: 10.1190/1.3360313.
Administration; 2013. Meissner FF. Petroleum geology of the Bakken Formation,
Far ME, Hardage B. Inversion of elastic properties of fractured Williston Basin, North Dakota and Montana in The economic
rocks from AVOAz data Marcellus Shale example. Houston: geology of the Williston Basin: Montana Geological Society.
SEG; 2013. p 3133–3137. Williston Basin Symposium; 1978.
Far ME, Sayers CM, Thomsen L, Han DH, Castagna JP. Seismic Momper JA. (1978). Oil migration limitations suggested by geo­
characterization of naturally fractured reservoirs using logical and geochemical considerations. In Physical Constraints
amplitude versus offset and azimuth analysis. Geophys Prospect on Petroleum Migration, AAPG, 1, B1‐B60.
2013;61 (2):427–447. Nishizawa O. Seismic velocity anisotropy in a medium containing
Ghorbani A, Zamora M, Cosenza P. Effects of desiccation on the oriented cracks – transversely isotropic case. J Phys Earth
elastic wave velocities of clay‐rocks. Int J Rock Mech Min Sci 1982;30:331–347.
2009;46:1267–1272. Panahi H, Kobchenko M, Renard F, Mazzini A, Scheibert J, Dysthe
Goodway B, Perez M, Varsek J, Abaco C. Seismic petrophysics and D, Jamtveit B, Malthe‐Sorenssen A, Meakin P. A 4D synchro­
isotropic‐anisotropic AVO methods for unconventional gas tron X‐ray‐tomography study of the formation of hydrocarbon‐
exploration. The Leading Edge 2010;29:1500–1508. migration pathways in heated organic‐rich shale. Spe J 2013;18
Hashin Z, Shtrikman S. A variational approach to the theory of the (2):366–377.
elastic behaviour of multiphase materials. J Mech Phys Solids Parney B, Williams M, Jenner E. Azimuthal NMO as an indicator
1963;11 (2):127–140. of natural fracturing Canadian Society of Exploration
Hemsing D. Laboratory determination of seismic anisotropy in Geophysicists, Expanded Abstracts; 2004. pp. S035–S035.
sedimentary rock from the Western Canadian Sedimentary Patrusheva N, Lebedev M, Pervukhina M, Dautriat J, Dewhurst
Basin, University of Alberta. M.S. thesis; 2007. DN. Changes in microstructure and elastic properties of Mancos
Hornby BE. Experimental laboratory determination of the dynamic shale after pyrolysis, in 76th EAGE Conference & Exhibition
elastic properties of wet, drained shales. J Geophys Res edited, EAGE, Amsterdam; 2014.
1998;103:29945–29964. Pervukhina M, Gurevich B, Dewhurst DN, Siggins AF.
IEA. Resources to Reserves. Paris: International Energy Agency; Experimental verification of the physical nature of velocity‐
2013. stress relationship for isotropic porous rocks. Geophys J Int
Johnston JE, Christensen NI. Seismic anisotropy of shales. 2010;181:1473–1479.
J Geophys Res 1995;100 (B4):5991–6003. Pervukhina M, Gurevich B, Golodoniuc P, Dewhurst DN.
Kobchenko M, Panahi H, Renard F, Dysthe DK, Malthe‐Sorenssen Parameterization of elastic stress sensitivity in shales. Geophysics
2011;76 (3):B1–B9.
A, Mazzini A, Scheibert J, Jamtveit B, Meakin P. 4D imaging of
fracturing in organic‐rich shales during heating. J Geophys Res Peters KE, Walters CC, Moldowan JM. The Biomarker Guide.
2011;116:B12201. Volume 2, Cambridge: Cambridge University Press; 2004.
Krief M, Garat J, Stellingwerff J, Ventre J. A petrophysical inter­ Biomarkers and Isotopes in Petroleum Systems and Earth
History.
pretation using the velocities of P and S waves (full‐waveform
sonic). The Log Analyst 1990;31(Nov):355–369. Price LC, Ging T, Daws T, Love A, Pawlewicz M, Anders D.
Lewan MD. Evaluation of Petroleum Generation by Hydrous Organic metamorphism in the Mississippian‐Devonian
Bakken Shale, N. Dakota portion of the Williston Basin. In:
Pyrolysis Experimentation. Philos Trans A Math Phys Eng Sci Woodward F, Meissner F, Clayton LJ, editors. Hydrocarbon
1985;315 (1531):123–134. Source Rocks of the Greater Rocky Mountain Region.
Lewan MD. Petrographic study of primary petroleum migration in Denver: Rock Mountain association of Geologists; 1984.
the woodford Shale and related rock units. In: Doligez B, editor. p 83–133.
Migration of Hydrocarbons in Sedimentary Basins. Paris: Ruud BO, Jakobsen M, Johansen TA. Seismic properties of shales
Editions Technip; 1987. p 113–190. during compaction. In SEG Technical Program Expanded
Lewan MD, Winters JC, Mcdonald JH. Generation of oil‐like Abstracts, Dallas, TX; 2003. pp. 1294–1297. doi: 10.1190/
pyrolyzates from organic‐rich shales. Science 1979;203 1.1817522
(4383):897–899. Saxena N, Mavko G, Mukerji T. Change in effective bulk mod­
Løseth H, Wensaas L, Gading M, Duffaut K, Springer M. Can ulus upon fluid or solid substitution. Geophysics 2013;78:
hydrocarbon source rocks be identified on seismic data? L45–L56.
Geology 2011;39 (12):1167–1170. Sayers CM. The effect of kerogen on the elastic anisotropy of
Lucier AMH, Hofmann R, Bryndzia LT. Evaluation of variable organic‐rich shales. Geophysics 2013a;78 (2):D65–D74.
gas saturation on acoustic log data from the Haynesville Shale Sayers CM. The Effect of Kerogen on the AVO Response
gas play. NW Louisiana: The Leading Edge; 2011 March. of Organic‐Rich Shales SEG. Houston (TX): SEG; 2013b.
pp 300–311.
p 2762–2766.