陕北英旺探区延长组长8储层特征研究
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摘要
本文综合应用沉积学、石油地质学、储层地质学等理论和方法,通过野外剖面观察、钻井岩心观察、测井资料解释、薄片鉴定、扫描电镜和储层岩性物性分析等手段,对英旺探区延长组的沉积相及储层特征进行了较为深入的研究。
研究区长8地层沉积体系类型主要为三角洲沉积体系和湖泊沉积体系。三角洲水下分流河道是长8油气储集的骨架砂体,砂体的发育完全受控于沉积相的展布,均呈北东一南西方向条带状展布。
英旺探区延长组砂岩主要为岩屑长石细砂岩和长石细砂岩,主要胶结物为绿泥石膜、方解石和自生石英。成岩作用主要为压实作用、胶结作用和溶蚀作用,成岩作用普遍进入晚成岩A期—晚成岩B期。
研究区主要孔隙类型为残余粒间孔、溶蚀粒间孔和粒内溶蚀孔。长8砂岩孔喉组合为小孔中细喉型、小孔细喉型和细孔微细喉型,孔隙度平均为6.93%,渗透率平均为0.65×10~(-3)μm~2,储集体为低孔、低渗储层。
英旺探区延长组储层性质主要受控于构造作用、沉积相和成岩作用三大因素。研究区地质结构简单,构造平缓,构造运动对储层物性影响有限;延长组砂岩具有粒径细、成分成熟度低和结构成熟度高的特点,这决定其物性较差;再者延长组储层经历了较长时间和较高强度的压实与胶结作用,且裂缝也不发育。由此可见,研究区是典型的低孔特低渗储集岩。
参照前人的分类标准并综合分析英旺探区储层物性特征,将本区储层划分为四类,其中长8有少量属于Ⅳ类储层,多数属于Ⅲ类储层。通过油藏控制因素和油气富集规律分析,认为英旺探区延长组具有利的生储盖组合和良好的油气圈闭条件。综合产能特征和测井资料在英旺探区延长组长8~3、长8~2两个含油层位优选出三类油气有利区块,为下一步勘探开发提供地质依据。
Applied with outcrop observation, core description, geophysical logging interpretation, thin section determination, Scanning Electron Microscope,reservoir lithology and physical property analysis and other analytic machinery,the sedimentary facies and micro-characteristic of Yanchang Formation in Yingwang exploration area are studied deeply.
Sedimentary systems of the Chang8 in Yingwang exploration area can be divided into delta and lacustrine facies.Subaquous distributary channel in delta front microfacies is identified, which is the main reservoir sand bodies for oil and gas of Chang 8.The distribution of sand bodies distributed from northeast to southwest are dominated by sedimentary facies.
Feldspar-lithic fine-sandstone and feldspar fine-sandstone are mainly sandstone of Yanchang Formation in Yingwang exploration area,and its diagenetic mineral includes chlorite films,calcite and autogeny-quartz etc. The diagensis is mainly compaction ,cementation and dissolution.All the sandstones have entered A period of late diagentic and B period of late diagentic stage.
The main pore types are remnant intergranular porosity,intergranular dissolution porosity and intragrnular dissolution porosity.Chang 8 pore textures are 6.93%.The average porosits is 0.65×10~(-3)μm~2. So Chang 8 is low-pore and low-permeability reservoir.
Reservoir properties are mainly controlled by tectonics, sedimentary facies and diagenesis. Because of simple configuration,gentle structure,the effect of the tectonic movement is relatively limited.The reservoir sandstone of Yangchang Formation has the characteristics of fine grain size,low compositional maturity and high textural maturity,determining the physical property of sandstone is bad.The reservoir of Yangchang Formation experienced longer and stronger compaction and cementation,and its fissure is undeveloped.In summary, reservoir sandstone of Chang 8 in the area is typical of low porosity and low permeability.
By looking for sand body and higher pore and higher permeability area, combined with oil product characteristic and electromotive curve data, three advantageous blocks of oil are predicted of different oi-bearing beds of Yanchang Formation in Yingwang exploration area, which provide the credibility geology gist for further exploration and exploitation in this area.
研究区长8地层沉积体系类型主要为三角洲沉积体系和湖泊沉积体系。三角洲水下分流河道是长8油气储集的骨架砂体,砂体的发育完全受控于沉积相的展布,均呈北东一南西方向条带状展布。
英旺探区延长组砂岩主要为岩屑长石细砂岩和长石细砂岩,主要胶结物为绿泥石膜、方解石和自生石英。成岩作用主要为压实作用、胶结作用和溶蚀作用,成岩作用普遍进入晚成岩A期—晚成岩B期。
研究区主要孔隙类型为残余粒间孔、溶蚀粒间孔和粒内溶蚀孔。长8砂岩孔喉组合为小孔中细喉型、小孔细喉型和细孔微细喉型,孔隙度平均为6.93%,渗透率平均为0.65×10~(-3)μm~2,储集体为低孔、低渗储层。
英旺探区延长组储层性质主要受控于构造作用、沉积相和成岩作用三大因素。研究区地质结构简单,构造平缓,构造运动对储层物性影响有限;延长组砂岩具有粒径细、成分成熟度低和结构成熟度高的特点,这决定其物性较差;再者延长组储层经历了较长时间和较高强度的压实与胶结作用,且裂缝也不发育。由此可见,研究区是典型的低孔特低渗储集岩。
参照前人的分类标准并综合分析英旺探区储层物性特征,将本区储层划分为四类,其中长8有少量属于Ⅳ类储层,多数属于Ⅲ类储层。通过油藏控制因素和油气富集规律分析,认为英旺探区延长组具有利的生储盖组合和良好的油气圈闭条件。综合产能特征和测井资料在英旺探区延长组长8~3、长8~2两个含油层位优选出三类油气有利区块,为下一步勘探开发提供地质依据。
Applied with outcrop observation, core description, geophysical logging interpretation, thin section determination, Scanning Electron Microscope,reservoir lithology and physical property analysis and other analytic machinery,the sedimentary facies and micro-characteristic of Yanchang Formation in Yingwang exploration area are studied deeply.
Sedimentary systems of the Chang8 in Yingwang exploration area can be divided into delta and lacustrine facies.Subaquous distributary channel in delta front microfacies is identified, which is the main reservoir sand bodies for oil and gas of Chang 8.The distribution of sand bodies distributed from northeast to southwest are dominated by sedimentary facies.
Feldspar-lithic fine-sandstone and feldspar fine-sandstone are mainly sandstone of Yanchang Formation in Yingwang exploration area,and its diagenetic mineral includes chlorite films,calcite and autogeny-quartz etc. The diagensis is mainly compaction ,cementation and dissolution.All the sandstones have entered A period of late diagentic and B period of late diagentic stage.
The main pore types are remnant intergranular porosity,intergranular dissolution porosity and intragrnular dissolution porosity.Chang 8 pore textures are 6.93%.The average porosits is 0.65×10~(-3)μm~2. So Chang 8 is low-pore and low-permeability reservoir.
Reservoir properties are mainly controlled by tectonics, sedimentary facies and diagenesis. Because of simple configuration,gentle structure,the effect of the tectonic movement is relatively limited.The reservoir sandstone of Yangchang Formation has the characteristics of fine grain size,low compositional maturity and high textural maturity,determining the physical property of sandstone is bad.The reservoir of Yangchang Formation experienced longer and stronger compaction and cementation,and its fissure is undeveloped.In summary, reservoir sandstone of Chang 8 in the area is typical of low porosity and low permeability.
By looking for sand body and higher pore and higher permeability area, combined with oil product characteristic and electromotive curve data, three advantageous blocks of oil are predicted of different oi-bearing beds of Yanchang Formation in Yingwang exploration area, which provide the credibility geology gist for further exploration and exploitation in this area.
引文
1.何自新,贺静.鄂尔多斯盆地中生界图册[M].北京:石油工业出版社,2004
2.宋国初,罗绍伦,张世富,等.陕甘宁盆地中生界陆相油田地质规律与勘探经验.长庆研究院报告,1993,内部资料
3.裘亦楠.中国陆相碎屑岩储层沉积学的进展[J].沉积学报1992,10(3):16-24
4.Tillman R.W.etal eds,Reservoir Sedimentology,1987,SEPM Spec.Publ.No.40
5.裘亦楠等.松辽陆相湖盆河流-三角洲各种沉积砂体的油水运动特点[J].1980,石油学报增刊,73-94
6.柳益群,李文厚.陕甘宁盆地东部上三叠统含油长石砂岩的成岩特点及孔隙演化[J].沉积学报,1996,14(3):87-95
7.罗静兰,J.Marcelo Ketzer,李文厚,阎世可,武富礼,李玉宏.延长油区侏罗系-上三叠统层序地层与生储盖组合[J].石油与天然气地质,2001,22(4):337-341
8.罗静兰,S.Morad,阎世可,武富礼,李玉宏,薛军民,张晓莉.河流-湖泊三角洲相砂岩成岩作用的重建及其对储层物性演化的影响-以延长油区侏罗系-上三叠统砂岩为例.中国科学(D辑)[J].2001,31(12):1006-1016
9.罗静兰,张晓莉,张云翔,李玉宏,武富礼.成岩作用对河流-三角洲相砂岩储层物性演化的影响-以延长油区上三叠统延长组长2砂岩为例[J].沉积学报,2001,19(4):541-547
10.黄思静,武文慧,刘洁等,大气水在碎屑岩次生孔隙形成中的作用-以鄂尔多斯盆地三叠系延长组为例[J].地球科学-中国地质大学学报,2003,28(4)419-424
11.顾家裕,张兴阳.油气沉积学发展回顾和应用现状[J].沉积学报,2003.21(1),137-141
12.田在艺,张庆春.中国含油气盆地岩相古地理与油气[M].北京:地质出版社,1997
13.李文厚,张小莉,刘生福等.鄂尔多斯盆地南部延长组主要油层组沉积相研究,1999,内部资料
14.李文厚.川口油田长6油层组沉积相特征与储集条件[J].西北大学学报.1996,26(2):155-158
25.李文厚.川口油田长6油层组储集层特征与油气富集规律[J].岩石学报.1998,14(1):117-127
16.梅志超.沉积相与古地理重建[M].西安:西北大学出版社,1994
17.杨华,付金华,喻建.陕北地区大型三角洲油藏富集规律及勘探技术应用.石油学报[J].2003,24(3):6-10
18.朱国华.陕甘宁盆地西南部上三叠统延长统低渗透砂岩和次生孔隙砂体的形成[J].沉积学报,1985,3(2):1-16.
19.朱国华,王文炯.论陕北安塞延长组三角洲的油气富集条件.石油与天然气地质.1987,8(4):440-447
20.柳益群,李文厚,冯乔..鄂尔多斯盆地东部上三叠统含油砂岩的古地温及成岩阶段[J].地质学报,1997,71(1):65-74
21.李志伟,刘颖梅.安塞油田长2、长3浅油层特征研究[J].低渗透油气田,2000,5(2):14-18
22.牟泽辉.鄂尔多斯盆地庆阳以南三叠系延长组长5、长6、长7储层成岩作用[J].天然气工业,2001,21(2):13-17
23.杨晓萍,陈丽华.陕北斜坡延长统低渗储集层成岩相研究[J].石油勘探与开发,2001,28(4),38-40
24.杨晓萍,裘择楠.鄂尔多斯盆地上三叠统延长组浊沸石的形成机理、分布规律与油气关系[J].沉积学报.2002,20(4):628-632
25.朱国华.陕北浊沸石次生孔隙砂体的形成与油气的关系[J].石油学报,1985,6(1)1-8
26.任继舜.印支运动及其在中国大地构造演化中的意义[J].中国地质科学院院报,第9号,1984,31-44
27.赵重远,汤锡元.鄂尔多斯地台西北部之白垩-第三纪地层[J].西北大学学报(自然科学版).1958,(2):49-55
28.张福礼,黄舜兴,杨昌贵,等.鄂尔多斯盆地天然气地质[M].北京:地质出版社,1994,33-65
30.杨俊杰,斐锡古.中国天然气地质学(卷四)鄂尔多斯盆地[M].北京:石油工业出版社,1996
31.赵重远.论含油气盆地的整体动态综合研究分析,见赵重远等主编,含油气盆地地质学研究进展[M].西安:西北大学出版社,1993
32.张渝昌.中国含油气盆地原型分析[M].南京大学出版社,1997
33.长庆油田石油地质志编写组,中国石油地质志(卷十二).北京:石油工业出版社,1992
34.王锡福.鄂尔多斯盆地区域地质背景及油气地质特征概述,见王锡福等主编,鄂尔多斯盆地地震油气勘探[M].北京:地质出版社,1992
35.王鸿祯.中国古地理图集.北京:中国地图出版社,1985
36.叶连俊,等.华北地台沉积建造[M].北京:科学出版社,1983
37.张抗.鄂尔多斯断块构造和资源[M].西安:陕西科学技术出版社,1989
38.赵重远,刘池阳.华北克拉通沉积盆地形成与演化及其油气赋存[M].西安:西北大学出版社,1990
39.夏青松,田景春,张锦泉,付金华,等.鄂尔多斯盆地陇东地区三叠系延长组长6-长8储层评价及有利区带预测[J].油气地质与采收率,2003,10(4):11-13
40.谢正温,谢渊,王剑等.富县地区延长组层序地层对储层的控制[J].矿物岩石,2004,24(2):95-103
41.杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002
42.梅志超,刘文荣.鄂尔多斯盆地三叠系长石砂岩中的自生浊沸石,见西北大学成立四十五周年学术报告会论文集(上集),1987
43.梅志超.沉积相与古地理重建[M].西安:西北大学出版社,1994
44.吴元燕,陈碧珏.、油矿地质学(第二版)[M].北京:石油工业出版社,1995,111-143
45.冯增昭.沉积岩石学(下册)[M].北京:石油工业出版社,1993,74-75
46.H.G.里丁.沉积环境和相[M].北京:科学出版社,1978,1-6
47.HangIUon DW,Morton A C,Todd S P.Developments in Sedimentay Provenance Studies.London,Oxford University Press,1991
48.曹守连,陈发景.塔里木盆地东北部沉积充填序列的物源分析[J].新疆石油地质,1994,15(2):126-131
49.汪正江,陈洪德,张锦泉.物源分析的研究与展望[J].沉积与特提斯地质,2000,20(4):104-110
50.闫义,林舸,王岳军等.盆地陆源碎屑沉积物对源区构造背景的指示意义[J].地球科学进展,2002,17(1):85-90
51.陈全红.鄂尔多斯盆地南部三叠系延长组沉积体系与层序地层学分析[D].西安:西北大学,2004
52.Morton A and Hurst A.Correlation of sandstones using heavy minerals:an example from the Statfjord Formation of the Snorrc Field,northern North Sea.In:Dunay R E,Hailwood E A,eds.Nonbiostratigraphical Methods of Dating and Correlation[C].Geological Society Special Publication,1995,89:3-22
53.李珍,焦养泉,刘春华等.黄骅坳陷高柳地区重矿物物源分析[J].石油勘探与开发,1998.25(6):5-7
54.何钟铧,刘招君,张峰.重矿物分析在盆地中的应用研究进展[J].地质科技情报,2001,20(4):29-32
55.陈纯芳,郑浚茂,王德发.板桥凹陷沙三段沉积体系与物源分析[J].古地理学报,2001,3(1):55-62
56.Knut Bjorlykke.1984.Formation of secondary porsity:How important is it? AAPG,Mcmoir37,175-207
57.华东石油学院岩矿教研室主编.沉积岩石学(下)[M].北京:石油工业出版社,1982,99-105
58.楼章华,兰翔,卢庆梅,蔡希源.地形、气候与湖面波动对浅水三角洲沉积环境的控制作用[J].沉积学报,1999,73(1):83-92
59.孙永传,李蕙生.碎屑岩沉积相及沉积环境[M].北京:地质出版社,1986,160-161
60.吴胜和,等著.油气储层地质学[M].北京:石油工业出版社,1998,155-172
61.Taylor J.C.M,Sandstones as reservoir rocks,Development in Petroleum Geology,1977,1:147-196
62.Tillam R.W.etal eds,Reservoir Sedimentology,1987,SEPM Spec.Publ.No.40
63.Folk RL.Petrology of sedimentary rocks[M].Austin:Hemphills,1968,170
64.谢渊,王剑,刘家铎,等著.鄂尔多斯盆地东南部延长租湖盆致密砂岩储层层序地层与油气勘探[M].北京:地质出版社,71-75
65.Franks S G,Forester R W.Relationships among secondary porosity,pore fluid chemistry and carbon dioxide,Texas Gulf Coast.M cDonald D A,Surdam & R C,Eds.Clastic Diageneis[C].America:AAPG Memoir 37,American Association of Petroleum Geologists,1984
66.Giles M R,Marshall J D.Constraints on the development of secondary porosity in the subsurface:Reevaluation of processes[J].Marine and Petroleum Geology,1986,3,243-255
67.Schmidt V,M cDonald D A.The role of secondary porosity in the course of sandstone diagenesis.Scholle,Schluger P.A P R,Eds Aspects of Diagenesis[C].America:SEPM Special Publication 29,Society of Economic,Paleontologists and Mineralogists,1979,175-255
68.Surdam R C,Boese S W,Crossey L J.The chemistry of secondary porosity.R Surdam C,McDonald D A.Eds.Clastic Diagenesis[C].America:AAPG Memoir 37,American Association of Petroleum Geologists,1984,127-149
69.Aase N E,BjΦrkum P A.The effect of graincoating microquartz on preserbation of reservoir porosity [J].AAPG Bulletin & Nadeau PH,1996,80:1654-1673
70.Bloch S,Lander R H,Bonell L.Anomalously high porosity and permeability in deeply buried sandstones reservoirs:Origin and predictability[J].AAPG Bulletin,2002,86:301-328
71.Jahren J,Ramm M.The porosity-preserving effects of Microcrystalline quartz coating in arenitic sandstones:Examples from the Norwegian continental shelf.Worden R H,Morad S,Eds.Quartz Cementation in Sandstones(29)[C].Oxford:Blackwell Special Publications of International Association of Sedimentologists,2000,271-280
72.Pottman E D,Larese R E,Heald M T,Clay coats:Occurrence and relevance to preservation of porosity in sandstones.Houseknecht D W,Pittman E D,Eds.Origin,Diagenesis,and petrophysics of Clay Minerals in Sandstones[C].America:SEPM special publication 47,Society of Economic Paleontolgists and Mineralogists,1992,241-264
73.赵澄林,刘孟慧.砂体微相和成岩作用[M].东营:华东石油学院出版社,1988,1-191
74.郑浚茂,庞明.碎屑储集岩的成岩作用研究[M].武汉:中国地质大学出版社,1989,53-129
75.林壬子,张金亮.陆相储层沉积学进展[M].北京:石油工业出版社,1996,97-127
76.刘宝珺,张锦泉.沉积成岩作用[M].北京:科学出版社,1992
77.王振奇,何振铭,徐龙,等.鄂尔多斯盆地葫芦河地区三叠系延长组低渗致密砂岩储层特征研究[J].江汉石油学院学报,1998,20(2):27-30
78.赵澄林,朱筱敏.沉积岩石学[M].北京:石油工业出版社,2000,34-36
79.李克勤主编.中国石油地质志(卷二十)[M].北京:石油工业出版社,1992
80.裘怿楠,薛叔浩.中国陆相油气储集层[M].北京:石油工业出版社,1997.158-219
81.陈安宁,韩永林,杨阳,等.鄂尔多斯盆地三叠系延长统成藏地质特征及油藏类型[A]见鄂尔多斯盆地油气勘探开发论文集,1990-2000[M].北京:石油工业出版社,2000.47-57
82.李文厚,张小莉,刘福生,等.鄂尔多斯盆地南部延长组主要油层组沉积相研究,1999,内部资料
83.杨华,张文正.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用:地质地 球化学特征[J].地球化学,2005,34(2):147-154
84.温爱琴,范久霄.鄂尔多斯盆地镇-泾地区三叠系烃源岩地化特征及勘探前景[J].河南石油,2003,17(2):15-17
85.陈安定.陕甘宁盆地中生界生油层特征-中国含油气盆地烃源岩评价[M].北京:石油工业出版社,1989
86.何自新,等著.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,1997
2.宋国初,罗绍伦,张世富,等.陕甘宁盆地中生界陆相油田地质规律与勘探经验.长庆研究院报告,1993,内部资料
3.裘亦楠.中国陆相碎屑岩储层沉积学的进展[J].沉积学报1992,10(3):16-24
4.Tillman R.W.etal eds,Reservoir Sedimentology,1987,SEPM Spec.Publ.No.40
5.裘亦楠等.松辽陆相湖盆河流-三角洲各种沉积砂体的油水运动特点[J].1980,石油学报增刊,73-94
6.柳益群,李文厚.陕甘宁盆地东部上三叠统含油长石砂岩的成岩特点及孔隙演化[J].沉积学报,1996,14(3):87-95
7.罗静兰,J.Marcelo Ketzer,李文厚,阎世可,武富礼,李玉宏.延长油区侏罗系-上三叠统层序地层与生储盖组合[J].石油与天然气地质,2001,22(4):337-341
8.罗静兰,S.Morad,阎世可,武富礼,李玉宏,薛军民,张晓莉.河流-湖泊三角洲相砂岩成岩作用的重建及其对储层物性演化的影响-以延长油区侏罗系-上三叠统砂岩为例.中国科学(D辑)[J].2001,31(12):1006-1016
9.罗静兰,张晓莉,张云翔,李玉宏,武富礼.成岩作用对河流-三角洲相砂岩储层物性演化的影响-以延长油区上三叠统延长组长2砂岩为例[J].沉积学报,2001,19(4):541-547
10.黄思静,武文慧,刘洁等,大气水在碎屑岩次生孔隙形成中的作用-以鄂尔多斯盆地三叠系延长组为例[J].地球科学-中国地质大学学报,2003,28(4)419-424
11.顾家裕,张兴阳.油气沉积学发展回顾和应用现状[J].沉积学报,2003.21(1),137-141
12.田在艺,张庆春.中国含油气盆地岩相古地理与油气[M].北京:地质出版社,1997
13.李文厚,张小莉,刘生福等.鄂尔多斯盆地南部延长组主要油层组沉积相研究,1999,内部资料
14.李文厚.川口油田长6油层组沉积相特征与储集条件[J].西北大学学报.1996,26(2):155-158
25.李文厚.川口油田长6油层组储集层特征与油气富集规律[J].岩石学报.1998,14(1):117-127
16.梅志超.沉积相与古地理重建[M].西安:西北大学出版社,1994
17.杨华,付金华,喻建.陕北地区大型三角洲油藏富集规律及勘探技术应用.石油学报[J].2003,24(3):6-10
18.朱国华.陕甘宁盆地西南部上三叠统延长统低渗透砂岩和次生孔隙砂体的形成[J].沉积学报,1985,3(2):1-16.
19.朱国华,王文炯.论陕北安塞延长组三角洲的油气富集条件.石油与天然气地质.1987,8(4):440-447
20.柳益群,李文厚,冯乔..鄂尔多斯盆地东部上三叠统含油砂岩的古地温及成岩阶段[J].地质学报,1997,71(1):65-74
21.李志伟,刘颖梅.安塞油田长2、长3浅油层特征研究[J].低渗透油气田,2000,5(2):14-18
22.牟泽辉.鄂尔多斯盆地庆阳以南三叠系延长组长5、长6、长7储层成岩作用[J].天然气工业,2001,21(2):13-17
23.杨晓萍,陈丽华.陕北斜坡延长统低渗储集层成岩相研究[J].石油勘探与开发,2001,28(4),38-40
24.杨晓萍,裘择楠.鄂尔多斯盆地上三叠统延长组浊沸石的形成机理、分布规律与油气关系[J].沉积学报.2002,20(4):628-632
25.朱国华.陕北浊沸石次生孔隙砂体的形成与油气的关系[J].石油学报,1985,6(1)1-8
26.任继舜.印支运动及其在中国大地构造演化中的意义[J].中国地质科学院院报,第9号,1984,31-44
27.赵重远,汤锡元.鄂尔多斯地台西北部之白垩-第三纪地层[J].西北大学学报(自然科学版).1958,(2):49-55
28.张福礼,黄舜兴,杨昌贵,等.鄂尔多斯盆地天然气地质[M].北京:地质出版社,1994,33-65
30.杨俊杰,斐锡古.中国天然气地质学(卷四)鄂尔多斯盆地[M].北京:石油工业出版社,1996
31.赵重远.论含油气盆地的整体动态综合研究分析,见赵重远等主编,含油气盆地地质学研究进展[M].西安:西北大学出版社,1993
32.张渝昌.中国含油气盆地原型分析[M].南京大学出版社,1997
33.长庆油田石油地质志编写组,中国石油地质志(卷十二).北京:石油工业出版社,1992
34.王锡福.鄂尔多斯盆地区域地质背景及油气地质特征概述,见王锡福等主编,鄂尔多斯盆地地震油气勘探[M].北京:地质出版社,1992
35.王鸿祯.中国古地理图集.北京:中国地图出版社,1985
36.叶连俊,等.华北地台沉积建造[M].北京:科学出版社,1983
37.张抗.鄂尔多斯断块构造和资源[M].西安:陕西科学技术出版社,1989
38.赵重远,刘池阳.华北克拉通沉积盆地形成与演化及其油气赋存[M].西安:西北大学出版社,1990
39.夏青松,田景春,张锦泉,付金华,等.鄂尔多斯盆地陇东地区三叠系延长组长6-长8储层评价及有利区带预测[J].油气地质与采收率,2003,10(4):11-13
40.谢正温,谢渊,王剑等.富县地区延长组层序地层对储层的控制[J].矿物岩石,2004,24(2):95-103
41.杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002
42.梅志超,刘文荣.鄂尔多斯盆地三叠系长石砂岩中的自生浊沸石,见西北大学成立四十五周年学术报告会论文集(上集),1987
43.梅志超.沉积相与古地理重建[M].西安:西北大学出版社,1994
44.吴元燕,陈碧珏.、油矿地质学(第二版)[M].北京:石油工业出版社,1995,111-143
45.冯增昭.沉积岩石学(下册)[M].北京:石油工业出版社,1993,74-75
46.H.G.里丁.沉积环境和相[M].北京:科学出版社,1978,1-6
47.HangIUon DW,Morton A C,Todd S P.Developments in Sedimentay Provenance Studies.London,Oxford University Press,1991
48.曹守连,陈发景.塔里木盆地东北部沉积充填序列的物源分析[J].新疆石油地质,1994,15(2):126-131
49.汪正江,陈洪德,张锦泉.物源分析的研究与展望[J].沉积与特提斯地质,2000,20(4):104-110
50.闫义,林舸,王岳军等.盆地陆源碎屑沉积物对源区构造背景的指示意义[J].地球科学进展,2002,17(1):85-90
51.陈全红.鄂尔多斯盆地南部三叠系延长组沉积体系与层序地层学分析[D].西安:西北大学,2004
52.Morton A and Hurst A.Correlation of sandstones using heavy minerals:an example from the Statfjord Formation of the Snorrc Field,northern North Sea.In:Dunay R E,Hailwood E A,eds.Nonbiostratigraphical Methods of Dating and Correlation[C].Geological Society Special Publication,1995,89:3-22
53.李珍,焦养泉,刘春华等.黄骅坳陷高柳地区重矿物物源分析[J].石油勘探与开发,1998.25(6):5-7
54.何钟铧,刘招君,张峰.重矿物分析在盆地中的应用研究进展[J].地质科技情报,2001,20(4):29-32
55.陈纯芳,郑浚茂,王德发.板桥凹陷沙三段沉积体系与物源分析[J].古地理学报,2001,3(1):55-62
56.Knut Bjorlykke.1984.Formation of secondary porsity:How important is it? AAPG,Mcmoir37,175-207
57.华东石油学院岩矿教研室主编.沉积岩石学(下)[M].北京:石油工业出版社,1982,99-105
58.楼章华,兰翔,卢庆梅,蔡希源.地形、气候与湖面波动对浅水三角洲沉积环境的控制作用[J].沉积学报,1999,73(1):83-92
59.孙永传,李蕙生.碎屑岩沉积相及沉积环境[M].北京:地质出版社,1986,160-161
60.吴胜和,等著.油气储层地质学[M].北京:石油工业出版社,1998,155-172
61.Taylor J.C.M,Sandstones as reservoir rocks,Development in Petroleum Geology,1977,1:147-196
62.Tillam R.W.etal eds,Reservoir Sedimentology,1987,SEPM Spec.Publ.No.40
63.Folk RL.Petrology of sedimentary rocks[M].Austin:Hemphills,1968,170
64.谢渊,王剑,刘家铎,等著.鄂尔多斯盆地东南部延长租湖盆致密砂岩储层层序地层与油气勘探[M].北京:地质出版社,71-75
65.Franks S G,Forester R W.Relationships among secondary porosity,pore fluid chemistry and carbon dioxide,Texas Gulf Coast.M cDonald D A,Surdam & R C,Eds.Clastic Diageneis[C].America:AAPG Memoir 37,American Association of Petroleum Geologists,1984
66.Giles M R,Marshall J D.Constraints on the development of secondary porosity in the subsurface:Reevaluation of processes[J].Marine and Petroleum Geology,1986,3,243-255
67.Schmidt V,M cDonald D A.The role of secondary porosity in the course of sandstone diagenesis.Scholle,Schluger P.A P R,Eds Aspects of Diagenesis[C].America:SEPM Special Publication 29,Society of Economic,Paleontologists and Mineralogists,1979,175-255
68.Surdam R C,Boese S W,Crossey L J.The chemistry of secondary porosity.R Surdam C,McDonald D A.Eds.Clastic Diagenesis[C].America:AAPG Memoir 37,American Association of Petroleum Geologists,1984,127-149
69.Aase N E,BjΦrkum P A.The effect of graincoating microquartz on preserbation of reservoir porosity [J].AAPG Bulletin & Nadeau PH,1996,80:1654-1673
70.Bloch S,Lander R H,Bonell L.Anomalously high porosity and permeability in deeply buried sandstones reservoirs:Origin and predictability[J].AAPG Bulletin,2002,86:301-328
71.Jahren J,Ramm M.The porosity-preserving effects of Microcrystalline quartz coating in arenitic sandstones:Examples from the Norwegian continental shelf.Worden R H,Morad S,Eds.Quartz Cementation in Sandstones(29)[C].Oxford:Blackwell Special Publications of International Association of Sedimentologists,2000,271-280
72.Pottman E D,Larese R E,Heald M T,Clay coats:Occurrence and relevance to preservation of porosity in sandstones.Houseknecht D W,Pittman E D,Eds.Origin,Diagenesis,and petrophysics of Clay Minerals in Sandstones[C].America:SEPM special publication 47,Society of Economic Paleontolgists and Mineralogists,1992,241-264
73.赵澄林,刘孟慧.砂体微相和成岩作用[M].东营:华东石油学院出版社,1988,1-191
74.郑浚茂,庞明.碎屑储集岩的成岩作用研究[M].武汉:中国地质大学出版社,1989,53-129
75.林壬子,张金亮.陆相储层沉积学进展[M].北京:石油工业出版社,1996,97-127
76.刘宝珺,张锦泉.沉积成岩作用[M].北京:科学出版社,1992
77.王振奇,何振铭,徐龙,等.鄂尔多斯盆地葫芦河地区三叠系延长组低渗致密砂岩储层特征研究[J].江汉石油学院学报,1998,20(2):27-30
78.赵澄林,朱筱敏.沉积岩石学[M].北京:石油工业出版社,2000,34-36
79.李克勤主编.中国石油地质志(卷二十)[M].北京:石油工业出版社,1992
80.裘怿楠,薛叔浩.中国陆相油气储集层[M].北京:石油工业出版社,1997.158-219
81.陈安宁,韩永林,杨阳,等.鄂尔多斯盆地三叠系延长统成藏地质特征及油藏类型[A]见鄂尔多斯盆地油气勘探开发论文集,1990-2000[M].北京:石油工业出版社,2000.47-57
82.李文厚,张小莉,刘福生,等.鄂尔多斯盆地南部延长组主要油层组沉积相研究,1999,内部资料
83.杨华,张文正.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用:地质地 球化学特征[J].地球化学,2005,34(2):147-154
84.温爱琴,范久霄.鄂尔多斯盆地镇-泾地区三叠系烃源岩地化特征及勘探前景[J].河南石油,2003,17(2):15-17
85.陈安定.陕甘宁盆地中生界生油层特征-中国含油气盆地烃源岩评价[M].北京:石油工业出版社,1989
86.何自新,等著.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,1997
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