Akinlua, A., Jarvie, D. M. Ajayi, T. R (2005) A pre appraisal of the application of Rock-Eval pyrolysis to source rock studies in the Niger Delta Journal of Petroleum Geology, 28: 39-48.
Bray, E. E., Foster, W. R (1980) A process for primary migration of petroleum. AAPG Bull, 64 (1): 107–114.
Bruce, C. H (1984) Smectite dehydration Its relation to structural development and hydrocarbon accumulation in northern Gulf of Mexico Basin. AAPG Bull, 68: 673–683.
Chanchani, J., Berg, R.R., Lee, C. I (1996) Pressure solution and microfracturing in primary oil migration, upper cretaceous Austin Chalk. Gulf Coast Assoc. Geol. Soc. Transact, 46: 71–78.
Craddock, P. R., Bake, K. D., Pomerantz, A. E (2018) Chemical, molecular, and microstructural evolution of kerogen during thermal maturation: case study from the Woodford Shale of Oklahoma, Energy & Fuels. ACS Publications, 32(4): 4859–4872.
Cordell, R. J (1973) Colloidal soap as proposed primary migration medium for hydrocarbons. AAPG Bull, 57 (9): 1618–1643.
Ding, W. L., Chao, L. Chunyan, X. Changchun, J., Kai, Z., Liming, W (2012) Fracture development in shale and its relationship to gas accumulation. Geoscience Frontiers, 3: 97-105.
Engelder, T., Lacazette, A (1990) Natural hydraulic fracturing. In: Proceedings of the International Symposium on Rock Joints, 4-6 June at Loen, Norway, p. 35–43.
England, W. A., Mackenzie, A. S., Mann, D. M., Quigley, T. M (1987) The movement and entrapment of petroleum fluids in the subsurface. J. Geol. Soc, 144 (2): 327–347.
Fawad, M., Mondol, N. H., Jahren, J., Bjorlykke, k (2010) Microfabric and rock properties of experimentally compressed sil-clay mixtures. Mar. Pet, 27: 1698-1712.
Figueroa Pilz, F., Dowey, P. J., Fauchille, A. L., Courtois, L., Bay, B., Ma, L., Taylor, K. G., Mecklenburgh, J., Lee, P. D (2017) Synchrotron tomographic quantification of strain and fracture during simulated thermal maturation of anorganic-rich shale, UK Kimmeridge Clay. J. Geophys. Res.: Solid Earth, 122: 2553–2564.
Glatz, G., Castanier, L. M., Kovscek, A. R (2016) Visualization and quantification of thermally induced porosity alteration of immature source rock using x-ray computed tomography. Energy Fuels, 30 (10): 8141–8149.
Goddard, D. A., Mancini, E. A., Talukar, S. C., Horn, M (1997) Bossier – Hanesvill shale, North Louisian salt basin: Lousiana State University, Baton Rouge, Louisiana, center for energy, pdf file, www. api. ning. com/files.
Goulart Teixeira, M., Donzé, F., Renard, F., Panahi, H., Papachristos, E., Scholtès, L (2017) Microfracturing during primary migration in shales. Tectonophysics, 694: 268–279.
Guo, X., He, S., Song, G., Wang, X. J., Wang, B. J., Na, L. I (2011) Evidences of over pressure caused by oil generation in Dongying depression. Earth Science Journal China Univ. Geosciences 36, 1085-1094 (in Chinese with English abstract).
Hill, D. G., Lombardi, T. E., Martin, J. P (2002) Fractured Shale Gas Potential in New York, Arvada, Colorado, pp. 1-16.
Hover, V. C., Peacor, D. R, and Walter, L. M (1996) Relationship between organic matter and authigenic illite in Devonian Black shales, Michigan and Illinois Basins, USA, siliciclastic diagenesis and fluidflow concepts and applications. SEM Spec. Publ, 55: 73-83.
Hunt, J. M (1996) Petroleum geochemistry and geology, 2nd edition. W. H. Freeman and Company. 743 pp.
Hunt, J. M (1990) Generation and migration of petroleum from abnormally pressured fluid compartments (1). AAPG Bull, 74 (1): 1–12.
Illing, V. C (1933) Migration of oil and natural gas. Inst. Petrol, 19 (114): 229-274.
Jahren, J., Haile, B. G., Hellevang, H., Bjřrlykke, E., Ohm, S. E (2013) Fracture patterns in organic rich mudstones-implications for primary petroleum migration. 75th EAGE Conference & Exhibition Incorporating SPE EUROPEC 2013 EAGE London, UK.
Jarvie, D. M., Hill, R. J., Ruble T. E., Pollastro, R. M (2007) Unconventional shale-gas systems: The Mississippian Barnett Shale of north-central Texas as one model for thermogenic shale-gas assessment. AAPG Bulletin, 91: 475-499.
Jin, Z. H., Johnson, S. E., Fan, Z. Q (2010) Subcritical propagation and coalescence of oilfilled cracks: getting the oil out of low-permeability source rocks. Geophys. Res. Lett. 37, L01305.
Kalani, M., Jahren, J., Mondol, N. H., Faleide, J. I (2015) Petrophysical implications of source rock microfracturing. Int. J. Coal Geol, 143: 43–67.
Kalani, M., Jahren, J., Mondol, N. H., Faleide, J. I (2015) Compaction processes and rock properties in uplifted clay dominated units - the Egersund Basin, Norwegian North Sea. Mar. Pet. Geol. (in press).
Kobchenko, M., Panahi, H., Renard, F., Dysthe, D.K., Malthe-Sørenssen, A., Mazzini, A., Scheibert, J., Jamtveit, B., Meakin, P (2011) 4D imaging of fracturing in organic-rich shales during heating. J. Geophys. Res. Solid Earth 116, B12201.
Lash, G. G., and Engelder, T (2005) An analysis of horizontal microcracking during catagenesis: example from the Catskill delta complex. AAPG Bull, 89 (11): 1433–1449.
Lafargue, W., Espitalie, J., Broks, T. M., Nyland, B (1994) Experimental simulation of primary migration. Org. Geochem, 22 (3–5): 575–586.
Lafargue, E., Marquis, F., Pillot, D (1998) Rock-Eval 6 applications in hydrocarbon exploration, production, and soil contamination studies. Rev. Inst. Fr. Petrol, 53(4): 421–437.
Leythaeuser, D., Littke, R., Radke, M., Schaefer, R. G (1988) Geochemical effects of petroleum migration and expulsion from Toarcian source rocks in the Hills syncline area, NW-Germany. Org. Geochem, 13: 489–502.
Li, D. H., J. Z. Li, S. J. Wang, and X. J (2009) Conditions of shale gas reservoir formation, Natural Gas Industry, 29(5): 22-26 (in Chinese with English abstract).
Ma, C. F., Dong, C. M., Luan, G. Q., Lin, C. Y., Liu, X, C., Elsworth, D (2016) Types, characteristics and effects of natural fluid pressure fractures in shale: a case study of the Paleogene strata in eastern China. Petroleum Explor. Dev, 43: 634-643.
Ma, C., Elsworth, D., Chunmei, D (2017) ‘Controls of hydrocarbon generation on the development of expulsion fractures in organic-rich shale: Based on the Paleogene Shahejie Formation in the Jiyang Depression, Bohai Bay Basin, East China’, Marine and Petroleum Geology. Elsevier, 86: 1406–1416.
McAuliffe, C. D (1979) Oil and gas migration–chemical and physical constraints. AAPG Bull, 63 (5): 761–781.
Montes-Hernandez, G., J. Duplay, L. Martinez, S. Escoffier and Rousset, D (2004) Structural modifications of Callovo-Oxfordian argillite under hydration/dehydration conditions. Applied Clay Science, 25: 187-194.
Nadeau, P. H (2011) Earth's energy “golden zone”: a synthesis from mineralogical research. Clay Miner, 46: 1–24.
Nadeau, P. H., Peacor, D. R., Yan, J., Hillier, S (2002) I–S precipitation in pore space as the cause of geopressuring in Mesozoic mudstones, Egersund Basin, Norwegian continental shelf. Am. Mineral, 87: 1580–1589.
Nelson, P. H (2009) Pore-throat sizes in sandstones, tight sandstones, and shales. AAPG Bulletin, 93: 329-340.
Nie, H. K., X. Tang, R. K. Bian (2009) Controlling factors for shale gas accumulation and prediction of potential development area in shale gas reservoir of South China. Acta Petrolei Sinica, 30(4): 484-491.
Ougier-Simonin, A., Renard, F., Boehm, C., Vidal-Gilbert, S (2016) Microfracturing and microporosity in shales. Earth Sci. Rev, 162: 198–226.
Panahi, H (2018) ‘In-situ imaging of fracture development during maturation of an organic-rich shale: Effects of heating rate and confinement’, Marine and Petroleum Geology, 95: 314–327.
Peters, K. E., and Cassa, M. R (1994) Applied source rock geochemistry. in: Magoon, L. B., Dow, W. G., (eds.), The petroleum system from source to trap. AAPG memoir, 60: 93-120.
Price, L. C (1989) Primary petroleum migration from shales with oxygen-rich organic matter. J. Petrol. Geol, 12 (3): 289–324.
Rudkiewicz, J. L., Brévart, O., Connan, J., Montel, F (1994) Primary migration behaviour of hydrocarbons: from laboratory experiments to geological situations through fluid flow models. Org. Geochem. 22 (3–5), 631IN7–639IN8.
Saif, T., Lin, Q., Bijeljic, B., Blunt, M. J (2017) a. Microstructural imaging and characterization of oil shale before and after pyrolysis. Fuel, 197: 562–574.
Saif, T., Lin, Q., Singh, K., Bijeljic, B., Blunt, M. J (2016) Dynamic imaging of oil shale pyrolysis using synchrotron X-ray microtomography. Geophys. Res. Lett, 43 (13): 6799–6807.
Snarskiy, A. N (1961) Relationship between primary migration and compaction of rocks. Petrol. Geol.: Digest of Russ. Lit. Petrol. Geol, 5: 362–365.
Storvoll, V., and Brevik, I (2008) Identifying time, temperature, and mineralogical effects on chemical compaction in shales by rock physics relations. Lead. Edge, 27: 750–756.
Tan, R. R (2009) Shale gas becomes the mainstay of the newly increased proven reserves, Natural Gas Industry, 1362: 29(5), 81 (in Chinese with English abstract).
Thyberg, B., Jahren, J., Winje, T., Bjørlykke, K., Faleide, J. I., Marcussen, Ø (2010) Quartz cementation in Late Cretaceous mudstones, northern North Sea: changes in rock properties due to dissolution of smectite and precipitation of micro-quartz crystals. Mar. Pet. Geol, 27: 1752–1764.
Tissot, B. P., and Welte, D. H (1978) Petroleum Formation and Occurrence. Springer-Verlag, New York, pp. 538.
Vernik, L (1994) Hydrocarbon-generation-induced microcracking of source rocks. Geophysics, 59 (4): 555–563.
Vidal, O., and B. Dubacq (2009) Thermodynamic modelling of clay dehydration, stability and compositional evolution with temperature, pressure and H20 activity, Geochmimica et Cosmochimica Acta, 73: 6544-6564.
Vidal, O., and B. Dubacq (2009) Thermodynamic modelling of clay dehydration, stability and compositional evolution with temperature, pressure and H20 activity, Geochmimica et Cosmochimica Acta, 73: 6544-6564.
Xu, C., Dowd, P. A. Tian, Z. F (2015) A simplified coupled hydro-thermal model for enhanced geothermal systems, Applied Energy. Elsevier, 140: 135–145.
Zeng, W., J. Zhang, W. Ding, S. Zhao, Y. Zhang, Z. Liu, K (2013) Fracture development in Paleozoic shale of Chongqing area (South China). Part one: Fracture characteristics and comparative analysis of main controlling factors. Journal of Asian Earth Sciences, 75: 251-266.
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