[1]. Zoback M.D., 2007. Reservoir Geomechanics, Cambridge University Press, Cambridge, New York. ##
[2]. Fellgett, M. W., Kingdon, A., Williams, J. D. O., and Gent, C. M. A. (2018). Stress magnitudes across UK regions: new analysis and legacy data across potentially prospective unconventional resource areas. Mar. Pet. Geol. 97, 24–31. ##
[3]. Nelson EJ, Meyer JJ, Hillis RR, Mildren SD (2005) Transverse drilling-induced tensile fractures in the West Tuna area, Gippsland Basin, Australia: implications for the in-situ stress regime, International Journal of Rock Mechanics and Mining Sciences, 42: 361–371. ##
[4]. Rider M H (2002) The geological interpretation of well logs, Second Edition, Rider-French Consulting Ltd. ##
[5]. خوشبخت ف، معماریان ح، محمدنیا م (1388) مقایسه شکستگی‌ها در یک موقعیت ساختاری یکسان در یک میدان نفتی، با استفاده از لاگ تصویری. فصل‌نامه علمی-پژوهشی علوم‌زمین، 19، 73: 65-70. ##
[6]. Tingay M, Reinecker J, Müller B (2008) Borehole breakout an drilling induced fracture analysis from image logs, World Stress Map Project, Guidelines, Image Logs, World Stress Map Project, 1: 8. ##
[7]. Assous S, Elkigton P, Clark S (2014) Automated detection of planar geological features in borehole images, Geophysics, 79, 1: 11–19, doi.org/10.1190/geo2013-0189.1. ##
[8]. Al-Rubaie A, Ben Mahmud H (2020) A numerical investigation on the performance of hydraulic fracturing in naturally fractured gas reservoirs based on stimulated rock volume, Journal of Petroleum Exploration and Production. ##
[9]. Allen M B, Armstrong H A (2008) Arabia–Eurasia collision and the forcing of mid-Cenozoic global cooling, Palaeogeogr. Palaeoclim, Palaeoecol, 265, 1–2: 52– 58, doi.org/10.1016/j.palaeo.2008.04.021. ##
[10]. Nelson R A (2001) Geologic analysis of naturally fractured reservoirs, Gulf Professional Publishing, United Kingdom, 332.
[11]. Talbot C J, Alavi M (1996) The past of a future syntaxis across the Zagros, Geological Society, London, Special Publications,100: 89-109, doi.org/10.1144/GSL.SP.1996.100.01.08. ##
[12]. Berberian M (1995) Master blind thrust faults hidden under the Zagros folds: active basement tectonics and surface morphotectonics, Tectonophysics, Tectonophysics, 241, 3-4: 193-224, doi.org/10.1016/0040-1951(94)00185-C. ##
[13]. Macleod J H (1972) Geological Map of Mehran, Scale 1:100,000. NIOC New York. ##
[14]. Gassemi M, Asadollah S (2015) Active surface cracking in Aghajari Formation of the Azar oil field, Zagros, western Iran, Marine and Petroleum Geology, 68: 498-508, doi.org/10.1016/j.marpetgeo.2015.09.011. ##
[15]. Geolog Tutorial of GEOLOG Software, the USA. ##
[16]. Bellahsen N, Fiore P, Pollard D D (2006) The role of fractures in the structural interpretation of Sheep Mountain Anticline, Wyoming, Journal of Structural Geology, 28, 5: 850-867, doi.org/10.1016/j.jsg.2006.01.013. ##
[17]. Ameen M S, Buhidma I M, Rahim Z (2010) The function of fractures and in-situ stresses in the Khuff reservoir performance, onshore fields, Saudi Arabia, AAPG Bull, 94, 27: 60. ##
[18]. Price N (1966) Fault and joint development in brittle and semi-brittle rock, Pergamon Press, Oxford, 176. ##
[19]. Price N, Cosgrove J (1990) Analysis of Geological Structures, Cambridge University Press, Cambridge, 502. ##
[20]. Falcon N L (1969) Problems of the relationship between surface structure and deep displacements illustrated by the Zagros range, In: P. KENT, G. Satterthwaite and A. SPENCER (Eds.), Time and Place Orogeny, Geological Society of London, 3: 9-22, doi.org/10.1144/GSL.SP.1969.003.01.0. ##
[21]. Stocklin J (1974) Possible ancient continental margins in Iran, In: C. BURK and C. DRAKE (Eds.), Geology of Continental Margins, Springer-Verlag, New York, 873-877. ##
[22]. Haynes S J, McQuillan H (1974) Evolution of the Zagros suture zone, southern Iran, Geological Society of America Bulletin, 85, 5: 739-744, doi.org/10.1130/0016-7606(1974)85<739:EOTZSZ>2.0.CO;2. ##
[23]. Stoneley R (1981) The geology of the Kuh-e Dalneshin area of southern Iran, and its bearing on the evolution of southern Tethys, Journal of the Geological Society London, 138, 5: 509-526. ##
[24]. Alavi M (1994)Tectonicsof the Zagros orogenic belt of Iran: new data and interpretations, Tectonophysics, 229, 3-4: 211-238, doi.org/10.1016/0040-1951(94)90030-2. ##
[25]. Stoecklin J (1968) Structural history and tectonics of Iran: a review, AAPG bulletin, 52, 7: 1229-1258, doi.org/10.1306/5D25C4A5-16C1-11D7-8645000102C1865D. ##
[26]. باسره م، فرضی‌پور ع، صفایی ه، خانه‌زر ر (1391) تأثیر وضعیت پی‌سنگ بر ساختارهای سطحی مجاور گسل بالارود در کمربند چین‌خورده رانده زاگرس براساس مدل‌سازی تجربی تکتونیکی، سی و یکمین گردهمایی علوم‌زمین، 9. ##
[27].شوراب, یوسفی موسوی (2018) تحلیل توسعه شکستگی‌ها وابسته به چین خوردگی و تعیین جهت تنش‌های برجا در سازند سروک در یکی از میادین نفتی غرب. زمین ساخت، 2، 6: 55-68. ##
[28]. Colman- Sad S P (1978) Fold development in Zagros simply fold belt, Southwest Iran, The American Association of petroleum Geologists Bulletin, 62, 6: 984-1003, doi.org/10.1306/C1EA4F81-16C9-11D7-8645000102C1865D. ##
[29]. Hessami K, Koyi H A, Talbot C J (2001b) The significance of strike slip faulting in the basement of the Zagros fold - thrust belt, Joumal of Petroleum Geology, 24, 1: 5-28. ##
[30]. Casini G, Gillespie P A, Verges J, Romaire I, Fernandez N, Casciello E, Saura E, Mehl C, Homke S, Embry J C, Aghajari L, Hunt D W (2011) Sub-seismic fractures in foreland fold and thrust belts: insight from the Lurestan Province, Zagros Mountains, Iran, Petroleum GeoscienceSearch Dropdown Menu, 17, 263e282, doi.org/10.1144/1354-079310-043. ##
[31]. Tavani S, Storti F, Soleimany B, Fallah M, Munoz J P, Gambini R (2011) Geometry, kinematics and fracture pattern of the Bangestan anticline, Zagros, SW Iran, Geological Magazine, 148, 5-6: 964-979. ##
[32]. Fard I A, Braathen A, Mokhtari M, Alavi S A (2006) Interaction of the Zagros fold thrust belt and the arabian-type, deep-seated folds in the Abadan Plain and the Dezful Embayment, SW Iran, Petroleum Geoscience, doi.org/10.1144/1354-079305-706. ##
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