大民屯静安堡西侧低潜山油气储层研究
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摘要
研究区位于辽河盆地大民屯凹陷西侧,研究区东侧于二十世纪八十年代发现了东胜堡、静安堡及曹台潜山,并已投入开发多年,其所处区域大民屯凹陷是一个周边为断层切割的三角形地堑式凹陷,属中新生代裂谷盆地,其发育和演化经历了地壳拱张,裂陷和坳陷三大地质发育阶段。基底则由太古界变质岩和元古界白云岩构成。其潜山构造格局主要受断裂构造控制。凹陷二级构造单元为呈北东向、凹隆相间、雁形排列的背斜、鼻状等构造带,大民屯静安堡西侧则位于静安堡断裂鼻状构造带西侧的低潜山带,与区域构造发育史有着紧密的联系。
由于低潜山埋藏较深,以往研究较少,因此以前研究主要局限于高潜山带。本文以构造地质、储层地质及油气藏地质的基本理论为指导,结合地震、测井资料对研究区域的地质背景和潜山构造特征、潜山储层特征进行了较详细的研究。通过对地震资料的精细解释,查清潜山顶面的构造形态,研究静安堡西侧低潜山带构造演化和圈闭的形成与演化规律。应用地质综合研究手段,查明潜山地层组成,岩石特征,储集空间及分布规律,研究裂缝的成因及发育规律,并在此基础上对研究区域的储层作出了评价,研究区裂缝发育程度以及储层发育以东部较好,向西部逐渐变差。
The research area is located in the west side of Damintun depression of Liaohe Basin.Dongsheng Fort, Jing'an Fort and Caotai buried have been found in the east side of the study area in 1980s,which have been put into development for many years.The Damintun depression is a circunferential fault cutting triangel-type depression,which belongs to Mesozoic-Cenozoic rift basin. Its development and evolution experienced three geological developed stages—crust uplifting,rifting and depression. The base lamina consists of Archean rocks and Proterozoiz dolomite. While the buried hill structure is mainly controlled by fault structure.The secondary depression structure units are North-East,concave and convex,nose-like anticlinal structural belt,which formed a goose-shaped arrangement,whereas,the west side of Damintun Jing'an Fort, situated in the zone of low buried hill of the west side of Jing'an fort fracture nose-like structure zone,has a close relationship with development history of regine structure.
As the zone of low buried hill deeply lies hidden in the earth,there were rare study of it before.The current study is mainly restricted to high buried hill zone,which has increased the difficult of research. Directed by the basic theory of structure geology,reservoir geology and oil and gas accumulation geogoly, as well as combining with earthquake and logging data, the geogoly backgound of the research area and the reservior characteristics of the buried hill have been studied in detail in this paper.Through the detailed interpretation of seiemic data,this paper is aimed to identify the structure form of the potential top surface of the buried hill,to study the structure evolution of the low buried hill zone in the west side of Jing'an Fort,and its form of the closed circle and the eveolution regular pattern.The paper also apply the comprehensive geoglogical study means to search out the composition of buried hill formation,rock features,storage space and distribution law,and then to study the causa of cracks and development law.Based on above,the evaluation to reserior area is that fractures development level and resrvior development to the east are well done,however,to the west it become worse.
由于低潜山埋藏较深,以往研究较少,因此以前研究主要局限于高潜山带。本文以构造地质、储层地质及油气藏地质的基本理论为指导,结合地震、测井资料对研究区域的地质背景和潜山构造特征、潜山储层特征进行了较详细的研究。通过对地震资料的精细解释,查清潜山顶面的构造形态,研究静安堡西侧低潜山带构造演化和圈闭的形成与演化规律。应用地质综合研究手段,查明潜山地层组成,岩石特征,储集空间及分布规律,研究裂缝的成因及发育规律,并在此基础上对研究区域的储层作出了评价,研究区裂缝发育程度以及储层发育以东部较好,向西部逐渐变差。
The research area is located in the west side of Damintun depression of Liaohe Basin.Dongsheng Fort, Jing'an Fort and Caotai buried have been found in the east side of the study area in 1980s,which have been put into development for many years.The Damintun depression is a circunferential fault cutting triangel-type depression,which belongs to Mesozoic-Cenozoic rift basin. Its development and evolution experienced three geological developed stages—crust uplifting,rifting and depression. The base lamina consists of Archean rocks and Proterozoiz dolomite. While the buried hill structure is mainly controlled by fault structure.The secondary depression structure units are North-East,concave and convex,nose-like anticlinal structural belt,which formed a goose-shaped arrangement,whereas,the west side of Damintun Jing'an Fort, situated in the zone of low buried hill of the west side of Jing'an fort fracture nose-like structure zone,has a close relationship with development history of regine structure.
As the zone of low buried hill deeply lies hidden in the earth,there were rare study of it before.The current study is mainly restricted to high buried hill zone,which has increased the difficult of research. Directed by the basic theory of structure geology,reservoir geology and oil and gas accumulation geogoly, as well as combining with earthquake and logging data, the geogoly backgound of the research area and the reservior characteristics of the buried hill have been studied in detail in this paper.Through the detailed interpretation of seiemic data,this paper is aimed to identify the structure form of the potential top surface of the buried hill,to study the structure evolution of the low buried hill zone in the west side of Jing'an Fort,and its form of the closed circle and the eveolution regular pattern.The paper also apply the comprehensive geoglogical study means to search out the composition of buried hill formation,rock features,storage space and distribution law,and then to study the causa of cracks and development law.Based on above,the evaluation to reserior area is that fractures development level and resrvior development to the east are well done,however,to the west it become worse.
引文
[1]许坤,潘耀丽,彭峰.辽河盆地下第三系层序分析[J]地层学杂志,1997,(04).27-31
[2]姚继峰,廖兴明,于天欣.辽河盆地构造分析[J]断块油气田,1995,(05).21-26
[3]孙素青,沈渭洲.大民屯凹陷沙河街组四段、三段层序特征及其与油气成藏条件之间的关系[J]地球学报,2006,(01).14-19
[4]林畅松,李思田,任建业.断陷湖盆层序地层研究和计算机模拟-以二连盆地乌里雅斯太断陷为例[J]地学前缘,1995,(03).124-131
[5]赵立旻,孙卉.大民屯凹陷西陡坡古近系岩性地层油气藏勘探[J]石油勘探与开发,2006,(03).309-314
[6]冉建斌,闫文华,杨长友,曹丽丽.大民屯凹陷层序格架及沉积体系[J]石油地球物理勘探,2005,(S1).56-60
[7]史彦尧,谢庆宾,彭仕宓,蒲秀刚,董良.大民屯凹陷沙四段层序地层与沉积体系研究[J]沉积与特提斯地质,2008,(01).33-38
[8]王祁军.大民屯凹陷西斜坡古近系岩性油藏预测技术与应用[J]特种油气藏,2006,(04).42-46
[9]王丹,陈永成,潘克,于兰.大民屯凹陷沙四段沉积体系特征及展布[J]特种油气藏,2007,(02).44-48
[10]史彦尧,谢庆宾,彭仕宓,蒲秀刚.大民屯凹陷沙四段层序地层学研究[J]西安石油大学学报(自然科学版),2007,(03).14-19
[11]黄鹤,田洋.大民屯凹陷古近系层序地层格架研究[J]石油天然气学报,2009,(03).62-67
[12]冯有良.大民屯凹陷沙四段-沙三段层序地层格架及岩性油气藏预测[J].岩性油气藏,2008,(04).
[13]谢文彦,姜建群,张占文,邱芳.大民屯凹陷油气系统研究[J].石油勘探与开发,2004,(02).15-18
[14]邱芳.大民屯凹陷基岩油气藏油气运聚规律研究[J].河南石油,2006,(03).1-8
[15]薛尚义.大民屯凹陷安福屯潜山油藏特征及油层分布[J].河南石油,2006,(01).8-13
[16]赵立旻,孙卉.大民屯凹陷西陡坡古近系岩性地层油气藏勘探[J].石油勘探与开发,2006,(03).309-314
[17]孙增玖,崔全章,向晟.大民屯凹陷东部陡坡带构造演化特征[J].石油地球物理勘探,2008,(03).63-69
[18]周晶,曹来圣,崔全章,孙增玖,李楠,杨长友,英紫娟,孙立志,汤昶.大民屯凹陷西斜坡Es_4段岩性油气藏整体解剖[J].石油地球物理勘探,2006,(S1)75-79
[19]郭彦民,李晓光,顾国忠,张瑞斌.大民屯凹陷元古界分布与储层预测方法[J].特种油气藏,2007,(02).27-31
[20]王泽权,孙立志,英紫娟,向晟,丁琼涛.大民屯凹陷再认识与重点勘探目标评价[J].石油地球物理勘探,2008,(S1).51-57
[21]冉建斌,闫文华,杨长友,曹丽丽.大民屯凹陷层序格架及沉积体系[J].石油地球物理勘探,2005,(S1).56-60
[22]陈永成,等.大民屯凹陷沙四段岩性油气藏勘探研究[M].沈阳：辽河科学技术出版社,2006：136-145.
[22]董敏煜.地震勘探[M].东营：石油大学出版社,2000：200--214.
[23]李玉君,等.地震信息在储层沉积微相随机建模中的应用[J].特种油气藏,2007,14(5)：4345.
[24]黄海平.李虹.马刊创.何会强大民屯凹陷高蜡油的形成条件[J]-石油与天然气地质2001(1).64-67
[25]张立新.李军.刘淑芝.张琳试析歧北凹陷异常压力在深层油气藏成藏过程中的控制作用[J]-石油勘探与开发2000(5).19-21
[26]卞应时,等.大港油田中浅层低阻油气层成因分析及评价[J].特种油气藏,21302,9(2)：26-28,
[27]吴元燕,陈碧珏.油矿地质学[M].北京：石油工业出版社,1996：108-110.
[28]陈绍生.单家增.许坤大民屯凹陷安福屯潜山带裂缝形成和演化的地球动力学特性分析[J]-石油勘探与开发2003(4)13-15
[29]罗宾巴瑟斯特碳酸盐沉积物及其成岩作用[M]北京：科学出版社,1977
[30]谢文彦.姜建群.张占文.邱芳大民屯凹陷油气系统研究[J]-石油勘探与开发2004(2).38-42
[31]赵良孝.祁勇碳酸盐岩储集层测井评价技术[M]北京：石油工业出版社,1994
[32]单家增.张占文.陈绍生.许坤大民屯凹陷安福屯潜山带古构造应力场与裂缝发育特征的光弹物理模拟实验研究[J]-石油勘探与开发2004(4).15-18
[33]葛许芳.唐瑾.吴郁.吴忠冀中坳陷河间南潜山油藏勘探技术[J]-石油勘探与开发2003(1).54-56
[34]王军.张强埕北30潜山太古宇储集层预测[J]-石油勘探与开发2003(1).57-59
[35]陈绍生.单家增.许坤大民屯凹陷安福屯潜山带裂缝形成和演化的地球动力学特性分析[期刊论文]-石油勘探与开发2003(4).13-15
[36]杨池银.张一伟黄骅地区叠合盆地演化与潜山油气聚集[J]-石油勘探与开发2003(6).21-24
[37]苏立萍.罗平.胡社荣苏桥潜山带奥陶系碳酸盐岩储集层研究[J]-石油勘探与开发2003(6).8-12
[38]郭建华,刘辰生,吴东胜等.大民屯凹陷静安堡西侧低潜山油气成藏条件分析[J].中南大学学报(自然科学版),2005,36(2)329-334
[39]郭建华.覃汉生.赵力民.芦天明轮南潜山构造油气藏与油气富集条件[J]-江汉石油学院学报1993(1).31-36
[40]袁先春.赵新国.刘小红.孙青.赵云峰东濮凹陷古潜山勘探潜力分析[J]-石油勘探与开发2001(2).29-32
[41]郑和荣.胡宗全渤海湾盆地及鄂尔多斯盆地上古生界天然气成藏条件分析[J]-石油学报2006(3).2-5
[42]李丕龙.张善文.王永诗多样性潜山成因、成藏与勘探--以济阳坳陷为例[M]北京：石油工业出版社,2003.
[43]李德生倾斜断块-潜山油气藏--拉张型断陷盆地内新的油气圈闭类型[J]石油与天然气地质1985(4).25-29
[44]谢文彦.姜建群.张占文.邱芳大民屯凹陷油气系统研究[J]-石油勘探与开发2004(2).38-42
[45].H. Asar and L.L. Handy, Influence of interfacial tension on gas/oil relative permeability in a gas-condense system. Soc. Pet. Eng. Reservoir Eng.(1988), pp. 257-264.
[46].E.W. Hough and G.L. Stegemeier, Correlation of surface and interfacial tension of light hydrocarbons in the critical region. Soc. Pet. Eng. J.(1961),pp. 259-263.
[47].J.A. Hugill and A.J. Van Welsenes, A simple correlation for natural gas+ condensate systems. Fluid Phase Equilibria 29(1986), pp.383-390.
[48].R.J.M. Huygens, D.M. Boersma, H.Ronde and J. Hagoort, Interfacial tension measurement of oil/water/steam systems using image processing techniques. SPE/DOE 24169(1992),pp.135-145.
[49].J.W. Jennings, An efficient method for the determination of interfacial tension from drop profiles. In:,American Chemical Society(1988), pp.959-967.
[50].F.J.M. Kalaydjian, J.C.Moulu and O.Vizika, Three phase flow in water-wet porous media:determination of gas/oil relative permeabilities under various spreading conditions. SPE 26671 1993), pp.689-700.
[51].D.L. Katz, R.R. Monroe, R.P. Trainer, Surface tension of crude oils containing dissolved gases, AIME, Technical Publications No.1624,pp.285-294.
[52].K.S.Pedersen, A. Fredenslund and P. Tomassen, Properties of oils and natural gases. In:,Gulf Publishing Company(1989), pp.196-207.
[53].S.T. Lee, M.C.H. Chien, A new multicomponent surface tension correlation based on scaling theory, SPE/DOE 12643 Fourth Symp.on EOR, Tulsa, OK, April 15-18.
[54].W. Sachs and V.Meyn, Pressure and temperature dependence of surface tension in the system natural gas/water. Colloids Surf.(1995), pp.291-301.
[55]S.Crampin, Implications of rock criticality for reservoir characterization, Journal of Petroleum Science and Engineering 24(1999), pp.29-48.
[56]A. Furrer, Complementarity Between Neutron and Synchrotron X-ray Scattering, World Scientific, Singapore(1998) (981-02-3558).
[57]T. Itakura, W.K. Bertram and R.B.Knott, The nano scale structural response of a natural kaolinitic clayey soil subjected to uniaxial compression, Journal of Applied Clay Science 29 (2005), pp.1-14.
[58]D.F.R. Mildner and P.L. Hall, Small-angle scattering from porous solids with fractal geometry, Journal of Physics.D, Applied Physics 19(1986), pp. 1535-1545.
[59]D.Prinz, W. Pyckhout-Hintzen and R. Littkea, Development of the meso-and macroporous structure of coals with rank as analysed with small angle neutron scattering and adsorption experiments, Fuel 83 (2004), pp.547-556.
[60]A.P. Radlinski, C.J. Boreham, G.D. Wignall and J.-S.Lin, Microstructural evolution of source rocks during hydrocarbon generation:a small-angle-scattering study, Physical Review B 53(1996) (21),pp. 14152-14160.
[61]A.P. Radlinski, E.Z. Radlinska, M. Agamalian, G.D.Wignall, P. Lindner and O.G. Randl, Fractal geometry of rocks, Physical Review Letters 82(1999)(15), pp. 3078-3081.
[62]A.P. Radlinski, E.Z. Radlinska, M. Agamalian, G.D. Wignall, P. Lindner and O.G. Randl, The fractal microstructure of ancient sedimentary rocks, Journal of Applied Crystallography 33 (2000), pp.860-862.
[63]A.P. Radlinski, C.J. Boreham, P. Lindner, O. Randl, G.D.Wignall, A. Hinde and J.M.Hope, Small angle neutron scattering signature of oil generation in artificially and naturally matured hydrocarbon source rocks, Organic Geochemistry 31 (2000), pp.1-14.
[64]T.M. Sabine and W.K. Bertram, The use of multiple-scattering data to enhance small-angle neutron scattering experiments, Acta Crystallographica A55(1999), pp.500-507.
[65]J. Schelten and W. Schmatz, Multiple-scattering treatment for small-angle scattering problems, Journal of Applied Crystallography 13(1980), pp.385-390.
[2]姚继峰,廖兴明,于天欣.辽河盆地构造分析[J]断块油气田,1995,(05).21-26
[3]孙素青,沈渭洲.大民屯凹陷沙河街组四段、三段层序特征及其与油气成藏条件之间的关系[J]地球学报,2006,(01).14-19
[4]林畅松,李思田,任建业.断陷湖盆层序地层研究和计算机模拟-以二连盆地乌里雅斯太断陷为例[J]地学前缘,1995,(03).124-131
[5]赵立旻,孙卉.大民屯凹陷西陡坡古近系岩性地层油气藏勘探[J]石油勘探与开发,2006,(03).309-314
[6]冉建斌,闫文华,杨长友,曹丽丽.大民屯凹陷层序格架及沉积体系[J]石油地球物理勘探,2005,(S1).56-60
[7]史彦尧,谢庆宾,彭仕宓,蒲秀刚,董良.大民屯凹陷沙四段层序地层与沉积体系研究[J]沉积与特提斯地质,2008,(01).33-38
[8]王祁军.大民屯凹陷西斜坡古近系岩性油藏预测技术与应用[J]特种油气藏,2006,(04).42-46
[9]王丹,陈永成,潘克,于兰.大民屯凹陷沙四段沉积体系特征及展布[J]特种油气藏,2007,(02).44-48
[10]史彦尧,谢庆宾,彭仕宓,蒲秀刚.大民屯凹陷沙四段层序地层学研究[J]西安石油大学学报(自然科学版),2007,(03).14-19
[11]黄鹤,田洋.大民屯凹陷古近系层序地层格架研究[J]石油天然气学报,2009,(03).62-67
[12]冯有良.大民屯凹陷沙四段-沙三段层序地层格架及岩性油气藏预测[J].岩性油气藏,2008,(04).
[13]谢文彦,姜建群,张占文,邱芳.大民屯凹陷油气系统研究[J].石油勘探与开发,2004,(02).15-18
[14]邱芳.大民屯凹陷基岩油气藏油气运聚规律研究[J].河南石油,2006,(03).1-8
[15]薛尚义.大民屯凹陷安福屯潜山油藏特征及油层分布[J].河南石油,2006,(01).8-13
[16]赵立旻,孙卉.大民屯凹陷西陡坡古近系岩性地层油气藏勘探[J].石油勘探与开发,2006,(03).309-314
[17]孙增玖,崔全章,向晟.大民屯凹陷东部陡坡带构造演化特征[J].石油地球物理勘探,2008,(03).63-69
[18]周晶,曹来圣,崔全章,孙增玖,李楠,杨长友,英紫娟,孙立志,汤昶.大民屯凹陷西斜坡Es_4段岩性油气藏整体解剖[J].石油地球物理勘探,2006,(S1)75-79
[19]郭彦民,李晓光,顾国忠,张瑞斌.大民屯凹陷元古界分布与储层预测方法[J].特种油气藏,2007,(02).27-31
[20]王泽权,孙立志,英紫娟,向晟,丁琼涛.大民屯凹陷再认识与重点勘探目标评价[J].石油地球物理勘探,2008,(S1).51-57
[21]冉建斌,闫文华,杨长友,曹丽丽.大民屯凹陷层序格架及沉积体系[J].石油地球物理勘探,2005,(S1).56-60
[22]陈永成,等.大民屯凹陷沙四段岩性油气藏勘探研究[M].沈阳：辽河科学技术出版社,2006：136-145.
[22]董敏煜.地震勘探[M].东营：石油大学出版社,2000：200--214.
[23]李玉君,等.地震信息在储层沉积微相随机建模中的应用[J].特种油气藏,2007,14(5)：4345.
[24]黄海平.李虹.马刊创.何会强大民屯凹陷高蜡油的形成条件[J]-石油与天然气地质2001(1).64-67
[25]张立新.李军.刘淑芝.张琳试析歧北凹陷异常压力在深层油气藏成藏过程中的控制作用[J]-石油勘探与开发2000(5).19-21
[26]卞应时,等.大港油田中浅层低阻油气层成因分析及评价[J].特种油气藏,21302,9(2)：26-28,
[27]吴元燕,陈碧珏.油矿地质学[M].北京：石油工业出版社,1996：108-110.
[28]陈绍生.单家增.许坤大民屯凹陷安福屯潜山带裂缝形成和演化的地球动力学特性分析[J]-石油勘探与开发2003(4)13-15
[29]罗宾巴瑟斯特碳酸盐沉积物及其成岩作用[M]北京：科学出版社,1977
[30]谢文彦.姜建群.张占文.邱芳大民屯凹陷油气系统研究[J]-石油勘探与开发2004(2).38-42
[31]赵良孝.祁勇碳酸盐岩储集层测井评价技术[M]北京：石油工业出版社,1994
[32]单家增.张占文.陈绍生.许坤大民屯凹陷安福屯潜山带古构造应力场与裂缝发育特征的光弹物理模拟实验研究[J]-石油勘探与开发2004(4).15-18
[33]葛许芳.唐瑾.吴郁.吴忠冀中坳陷河间南潜山油藏勘探技术[J]-石油勘探与开发2003(1).54-56
[34]王军.张强埕北30潜山太古宇储集层预测[J]-石油勘探与开发2003(1).57-59
[35]陈绍生.单家增.许坤大民屯凹陷安福屯潜山带裂缝形成和演化的地球动力学特性分析[期刊论文]-石油勘探与开发2003(4).13-15
[36]杨池银.张一伟黄骅地区叠合盆地演化与潜山油气聚集[J]-石油勘探与开发2003(6).21-24
[37]苏立萍.罗平.胡社荣苏桥潜山带奥陶系碳酸盐岩储集层研究[J]-石油勘探与开发2003(6).8-12
[38]郭建华,刘辰生,吴东胜等.大民屯凹陷静安堡西侧低潜山油气成藏条件分析[J].中南大学学报(自然科学版),2005,36(2)329-334
[39]郭建华.覃汉生.赵力民.芦天明轮南潜山构造油气藏与油气富集条件[J]-江汉石油学院学报1993(1).31-36
[40]袁先春.赵新国.刘小红.孙青.赵云峰东濮凹陷古潜山勘探潜力分析[J]-石油勘探与开发2001(2).29-32
[41]郑和荣.胡宗全渤海湾盆地及鄂尔多斯盆地上古生界天然气成藏条件分析[J]-石油学报2006(3).2-5
[42]李丕龙.张善文.王永诗多样性潜山成因、成藏与勘探--以济阳坳陷为例[M]北京：石油工业出版社,2003.
[43]李德生倾斜断块-潜山油气藏--拉张型断陷盆地内新的油气圈闭类型[J]石油与天然气地质1985(4).25-29
[44]谢文彦.姜建群.张占文.邱芳大民屯凹陷油气系统研究[J]-石油勘探与开发2004(2).38-42
[45].H. Asar and L.L. Handy, Influence of interfacial tension on gas/oil relative permeability in a gas-condense system. Soc. Pet. Eng. Reservoir Eng.(1988), pp. 257-264.
[46].E.W. Hough and G.L. Stegemeier, Correlation of surface and interfacial tension of light hydrocarbons in the critical region. Soc. Pet. Eng. J.(1961),pp. 259-263.
[47].J.A. Hugill and A.J. Van Welsenes, A simple correlation for natural gas+ condensate systems. Fluid Phase Equilibria 29(1986), pp.383-390.
[48].R.J.M. Huygens, D.M. Boersma, H.Ronde and J. Hagoort, Interfacial tension measurement of oil/water/steam systems using image processing techniques. SPE/DOE 24169(1992),pp.135-145.
[49].J.W. Jennings, An efficient method for the determination of interfacial tension from drop profiles. In:,American Chemical Society(1988), pp.959-967.
[50].F.J.M. Kalaydjian, J.C.Moulu and O.Vizika, Three phase flow in water-wet porous media:determination of gas/oil relative permeabilities under various spreading conditions. SPE 26671 1993), pp.689-700.
[51].D.L. Katz, R.R. Monroe, R.P. Trainer, Surface tension of crude oils containing dissolved gases, AIME, Technical Publications No.1624,pp.285-294.
[52].K.S.Pedersen, A. Fredenslund and P. Tomassen, Properties of oils and natural gases. In:,Gulf Publishing Company(1989), pp.196-207.
[53].S.T. Lee, M.C.H. Chien, A new multicomponent surface tension correlation based on scaling theory, SPE/DOE 12643 Fourth Symp.on EOR, Tulsa, OK, April 15-18.
[54].W. Sachs and V.Meyn, Pressure and temperature dependence of surface tension in the system natural gas/water. Colloids Surf.(1995), pp.291-301.
[55]S.Crampin, Implications of rock criticality for reservoir characterization, Journal of Petroleum Science and Engineering 24(1999), pp.29-48.
[56]A. Furrer, Complementarity Between Neutron and Synchrotron X-ray Scattering, World Scientific, Singapore(1998) (981-02-3558).
[57]T. Itakura, W.K. Bertram and R.B.Knott, The nano scale structural response of a natural kaolinitic clayey soil subjected to uniaxial compression, Journal of Applied Clay Science 29 (2005), pp.1-14.
[58]D.F.R. Mildner and P.L. Hall, Small-angle scattering from porous solids with fractal geometry, Journal of Physics.D, Applied Physics 19(1986), pp. 1535-1545.
[59]D.Prinz, W. Pyckhout-Hintzen and R. Littkea, Development of the meso-and macroporous structure of coals with rank as analysed with small angle neutron scattering and adsorption experiments, Fuel 83 (2004), pp.547-556.
[60]A.P. Radlinski, C.J. Boreham, G.D. Wignall and J.-S.Lin, Microstructural evolution of source rocks during hydrocarbon generation:a small-angle-scattering study, Physical Review B 53(1996) (21),pp. 14152-14160.
[61]A.P. Radlinski, E.Z. Radlinska, M. Agamalian, G.D.Wignall, P. Lindner and O.G. Randl, Fractal geometry of rocks, Physical Review Letters 82(1999)(15), pp. 3078-3081.
[62]A.P. Radlinski, E.Z. Radlinska, M. Agamalian, G.D. Wignall, P. Lindner and O.G. Randl, The fractal microstructure of ancient sedimentary rocks, Journal of Applied Crystallography 33 (2000), pp.860-862.
[63]A.P. Radlinski, C.J. Boreham, P. Lindner, O. Randl, G.D.Wignall, A. Hinde and J.M.Hope, Small angle neutron scattering signature of oil generation in artificially and naturally matured hydrocarbon source rocks, Organic Geochemistry 31 (2000), pp.1-14.
[64]T.M. Sabine and W.K. Bertram, The use of multiple-scattering data to enhance small-angle neutron scattering experiments, Acta Crystallographica A55(1999), pp.500-507.
[65]J. Schelten and W. Schmatz, Multiple-scattering treatment for small-angle scattering problems, Journal of Applied Crystallography 13(1980), pp.385-390.
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