川西地区上三叠统油气储层控制因素及评价研究
|
摘要
川西前陆盆地上三叠统须家河组碎屑岩储层是川西前陆盆地重要的勘探领域和层系之一,由于川西前陆盆地产层埋深较深,成岩作用程度较强,受长期挤压作用影响,故其储层多为低孔低渗的致密储层,非均质性强,物性差,勘探难度很大,因此深入研究其储层特征具有重要意义。
本文运用油气沉积学、储层地质学、矿物岩石学、地球化学以及储层评价等理论和方法技术,对川西前陆盆地上三叠统须家河组碎屑岩储层的岩石学特征、砂体成因类型及分布、成岩作用类型、孔隙类型及演化、物性特征及其影响因素等进行了深入的研究,取得了以下主要成果:
1.在川西前陆盆地中通过岩石薄片观察、扫描电镜以及电子探针分析,在须二段发现石英溶蚀现象,首次在研究区论证了石英溶蚀现象存在的合理性,指出了石英直接溶蚀发生的地区位置,分析了导致石英溶蚀发生的碱性流体的来源以及酸、碱溶蚀现象发生的顺序,量化了碱性溶蚀对储层物性的影响特征。
2.提出了一套有效的储层成岩相研究方法,即将成岩相研究与区域构造运动、沉积环境、盆地流体性质以及物源特征相结合,分析研究区主要单因素成岩相,再将各单因素成岩相进行有机叠加即可划分储层综合成岩相,建立成岩相与储层物性之间的因果关系。本次研究将川西前陆盆地须家河组储层划分为6种单因素成岩相和11种综合成岩相类型,提出影响须家河组储层的成岩相主要是绿泥石衬边、溶蚀和破裂成岩相、压实压溶、硅质胶结和碳酸盐胶结成岩相。
3.构造、沉积-层序和成岩作用综合控制了研究区优质储层的发育,在不同构造单元储层主控因素又有所差别:冲断带储层主要受构造裂缝控制;前渊坳陷带储层受裂缝和成岩作用控制;前缘斜坡带储层为沉积-层序及成岩作用控制;前陆隆起带受沉积-层序因素控制;优质储层主要发育于斜坡带和隆起带。
4.结合川西前陆盆地储层特征以及生产实际,制定储层评价与分类标准,对川西前陆盆地上三叠统碎屑岩储层进行评价与预测。指出层序Ⅱ低位域的优质储层主要分布在安岳-南充-潼南-磨溪一带;层序Ⅲ低位域的八角场-西充-潼南-磨溪一带。优质储层发育于三角洲前缘亚相,成岩相类型主要为压实-绿泥石衬边-溶蚀-破裂成岩相。
The reservoir of Xujiahe formation of the Upper Triassic clastic reservoir is one of the key stratum series in the western Sichuan foreland basin. Due to the pay formation was buried deeply and depressed for a long time, it is the reservoir with low porosity , low permeability and heterogeneous, which is very hard to explore. Therefore, it is necessary to make research into Xujiahe formation of the Upper Triassic reservoir characteristics.
Based on the theories and technologies of sedimentology, reservoir geology, petrology, geochemistry and reservoir evaluation, researches are carried out on several aspects such as reservoir petrologic characteristics, reservoir sandbody genesis types and distribution characteristics, diagenesis type, reservoir pore types and evolution, physical property characteristics and its controlling factors. The results are as follows:
(1) By the thin section observation, the analysis of the scanning electron microscope and the electron microprobe, it is thought reasonable that quartz direct dissolution exist in west Sichuan foreland basin of the Upper Triassic formation. The paper not only pointed out the area of quartz dissolution, analyzed the origion of alkaline fluid and the order of acidic and alkaline dissolution, but also quanized the effect of the alkaline dissolution to the reservoir characteristics.
(2) By combination of diagenetic facies study with regional structural movement, depositional environment, fluid characteristics and provenance property, the paper proposed the effective study method of reservoir diagenetic facies. The diagenetic single factor of reservoirs was analyzed in the western Sichuan foreland basin of the Upper Triassic. This paper determined the comprehensive diagenetic facies by superimposing the single factor diagenetic facies. The relationship of diagenetic facies and reservoir physical property was established. The reservoir of the Upper Triassic in the western Sichuan foreland basin can be divided into six kinds of single diagenetic facies and eleven kinds of comprehensive diagenetic facies. The mainly diagenetic facies which effect the reservoir characteristics include lining chlorite facies, dissolution facies, fracture facies, compaction-pressolution facies, quartz secondary enlargement facies and carbonate cementation facies.
(3) Based on the comprehensive analysis on the influence of structure, sequence– sedmient and diagenesis, worked out the chief controlling factors of reservoir property in different foreland structure: in thrust belts structure fracture were chief factor, in fore-deep fracture and diagenesis were necessary, in fore-slope the kinds of sand body were important,which were controled by sequence– sedmient and diagenesis, in fore-bulge sequence and sedmient were chief factors. The high quality reservoir mainly developed in fore-slope and fore-bulge belt.
(4) In the end, the clastic reservoir evaluation and prediction were performed in the different tectonic zones and different sequences of the Upper Triassic in the western Sichuan foreland basin on the base of sedimentary facies distribution, diagenesis facies, reservoir evolution mode, pore and permeability distribution ichnographies. SequenceⅡLST high quality reservoirs developed in Anyue, Nanchong, Tongnan and Moxi structure, SequenceⅢLST high quality reservoirs developed in Bajiaochang, Xichong, Tongnan and Moxi structure. Good reservoirs developed in delta front subfacies, with the kind of diagenetic facies series of compaction-lining chlorite-dissolution-fracture facies.
本文运用油气沉积学、储层地质学、矿物岩石学、地球化学以及储层评价等理论和方法技术,对川西前陆盆地上三叠统须家河组碎屑岩储层的岩石学特征、砂体成因类型及分布、成岩作用类型、孔隙类型及演化、物性特征及其影响因素等进行了深入的研究,取得了以下主要成果:
1.在川西前陆盆地中通过岩石薄片观察、扫描电镜以及电子探针分析,在须二段发现石英溶蚀现象,首次在研究区论证了石英溶蚀现象存在的合理性,指出了石英直接溶蚀发生的地区位置,分析了导致石英溶蚀发生的碱性流体的来源以及酸、碱溶蚀现象发生的顺序,量化了碱性溶蚀对储层物性的影响特征。
2.提出了一套有效的储层成岩相研究方法,即将成岩相研究与区域构造运动、沉积环境、盆地流体性质以及物源特征相结合,分析研究区主要单因素成岩相,再将各单因素成岩相进行有机叠加即可划分储层综合成岩相,建立成岩相与储层物性之间的因果关系。本次研究将川西前陆盆地须家河组储层划分为6种单因素成岩相和11种综合成岩相类型,提出影响须家河组储层的成岩相主要是绿泥石衬边、溶蚀和破裂成岩相、压实压溶、硅质胶结和碳酸盐胶结成岩相。
3.构造、沉积-层序和成岩作用综合控制了研究区优质储层的发育,在不同构造单元储层主控因素又有所差别:冲断带储层主要受构造裂缝控制;前渊坳陷带储层受裂缝和成岩作用控制;前缘斜坡带储层为沉积-层序及成岩作用控制;前陆隆起带受沉积-层序因素控制;优质储层主要发育于斜坡带和隆起带。
4.结合川西前陆盆地储层特征以及生产实际,制定储层评价与分类标准,对川西前陆盆地上三叠统碎屑岩储层进行评价与预测。指出层序Ⅱ低位域的优质储层主要分布在安岳-南充-潼南-磨溪一带;层序Ⅲ低位域的八角场-西充-潼南-磨溪一带。优质储层发育于三角洲前缘亚相,成岩相类型主要为压实-绿泥石衬边-溶蚀-破裂成岩相。
The reservoir of Xujiahe formation of the Upper Triassic clastic reservoir is one of the key stratum series in the western Sichuan foreland basin. Due to the pay formation was buried deeply and depressed for a long time, it is the reservoir with low porosity , low permeability and heterogeneous, which is very hard to explore. Therefore, it is necessary to make research into Xujiahe formation of the Upper Triassic reservoir characteristics.
Based on the theories and technologies of sedimentology, reservoir geology, petrology, geochemistry and reservoir evaluation, researches are carried out on several aspects such as reservoir petrologic characteristics, reservoir sandbody genesis types and distribution characteristics, diagenesis type, reservoir pore types and evolution, physical property characteristics and its controlling factors. The results are as follows:
(1) By the thin section observation, the analysis of the scanning electron microscope and the electron microprobe, it is thought reasonable that quartz direct dissolution exist in west Sichuan foreland basin of the Upper Triassic formation. The paper not only pointed out the area of quartz dissolution, analyzed the origion of alkaline fluid and the order of acidic and alkaline dissolution, but also quanized the effect of the alkaline dissolution to the reservoir characteristics.
(2) By combination of diagenetic facies study with regional structural movement, depositional environment, fluid characteristics and provenance property, the paper proposed the effective study method of reservoir diagenetic facies. The diagenetic single factor of reservoirs was analyzed in the western Sichuan foreland basin of the Upper Triassic. This paper determined the comprehensive diagenetic facies by superimposing the single factor diagenetic facies. The relationship of diagenetic facies and reservoir physical property was established. The reservoir of the Upper Triassic in the western Sichuan foreland basin can be divided into six kinds of single diagenetic facies and eleven kinds of comprehensive diagenetic facies. The mainly diagenetic facies which effect the reservoir characteristics include lining chlorite facies, dissolution facies, fracture facies, compaction-pressolution facies, quartz secondary enlargement facies and carbonate cementation facies.
(3) Based on the comprehensive analysis on the influence of structure, sequence– sedmient and diagenesis, worked out the chief controlling factors of reservoir property in different foreland structure: in thrust belts structure fracture were chief factor, in fore-deep fracture and diagenesis were necessary, in fore-slope the kinds of sand body were important,which were controled by sequence– sedmient and diagenesis, in fore-bulge sequence and sedmient were chief factors. The high quality reservoir mainly developed in fore-slope and fore-bulge belt.
(4) In the end, the clastic reservoir evaluation and prediction were performed in the different tectonic zones and different sequences of the Upper Triassic in the western Sichuan foreland basin on the base of sedimentary facies distribution, diagenesis facies, reservoir evolution mode, pore and permeability distribution ichnographies. SequenceⅡLST high quality reservoirs developed in Anyue, Nanchong, Tongnan and Moxi structure, SequenceⅢLST high quality reservoirs developed in Bajiaochang, Xichong, Tongnan and Moxi structure. Good reservoirs developed in delta front subfacies, with the kind of diagenetic facies series of compaction-lining chlorite-dissolution-fracture facies.
引文
1 顿铁军.储层研究状况与发展趋势向[J].西北地质,1995,16(2):1～15.
2 钱峥,赵澄林,刘孟慧. 济阳坳陷深层天然气致密砂岩储集空间成因[J]. 石油大学学报(自然科学版),1994,18(6):21～25.
3 赵澄林,等.储层沉积学[M]. 北京:石油工业出版社,1998.
4 朱国华,等.成岩作用与砂岩孔隙的演化[M].北京:石油工业出版社,1982.
5 西北大学地质系译. 碎屑岩的成岩作用(译文集)[M]. 西安:西北大学出版社,1986.
6 刘宝珺,张锦泉.沉积成岩作用[ M].北京:科学出版社. 1992, 622,68～92.
7 杨晓宁,陈洪德,寿建峰,等.碎屑岩次生孔隙形成机制[J].大庆石油学院学报, 2004, 28(1) : 4～6.
8 沃尔特·施密特.砂岩成岩过程中地次生储集孔隙[M].北京:石油工业出版社. 1982,272～276.
9 Boles, J.R. Secondary porosity reactions in the Stevens Sandstones, San Joaquin Valley,California. In:Clastic Diagenesis (Eds D.A.McDonald & R.C.Surdam). Memoir 37,American Association of Petroleum Geologists, Tulsa, OK.1984, 217~225.
10 Bj?rlykke,K. Formation of secondary porosity:How important is it? In:Clastic Diagenesis (Eds D.A.McDonald & R.C.Surdam). Memoir 37,American Association of Petroleum Geologists,Tulsa, ok. 1984,277~286.
11 Bloch,S. Secondary porosity in sandstones:Significance,origin,relationship to subaerial unconformities, and effect on predrill reservoir quality prediction. In: Reservoir Quality Assessment and Prediction in Clastic Rocks (Ed.M.D.Wilson). Short Course 30,Society of Sedimentary Geologist,Tulsa,OK. 1994,136~159.
12 黄思静,侯中键.地下孔隙度和渗透率在空间和时间上的变化及影响因素[J].沉积学报. 2001, 19(2) :224～230.
13 朱国华.陕北浊沸石次生孔隙砂体的形成与油气关系[J]. 石油学报. 1985, 6(1) :1～8.
14 寿建峰,朱国华.砂岩储层孔隙保存的定量预测研究[J]. 地质科学. 1998, 32(2) :224～249.
15 邱隆伟,姜在兴.陆源碎屑岩的碱性成岩作用[J]. 地质出版社. 2006, 1～2.
16 Bloch,S.,Lander, R.H. & Bonnell,L. Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Origin and predictability. American Association of Petroleum GeologistsBulletin. 2002,86:301~328.
17 Worden,R.H.& Burley,S.D. Sandstone diagenesis: the evolution of sand to stone. In: Sandstone Diagenesis: Recent and Ancient (Eds S.D.Burley & R.H. Worden). Reprint Series Volume 4 of the International Association of Sedimentologist. Blackwell Science, Oxford. 2003,3~44.
18 裘怿楠, 薛叔浩, 应凤祥. 中国陆相油气储集层[M]. 北京: 石油工业出版社,1997.
19 应凤祥, 罗平, 何东博,等. 中国含油气盆地碎屑岩储集层成岩作用与成岩数值模拟[M]. 北京: 石油工业出版社, 2004.
20 Bloch S. Secondary porosity in sandstones: significance, origion, relationship to subaerial uncomformities, and effect on predrill reservoir quality prediction[A]. in:Wilson M D,ed. Reservoir quality assessment and prediction in clastics rocks[C]. SEPM short Course, 1994, 30: 136~159.
21 陈丽华,赵澄林. 碎屑岩天然气储集层次生孔隙三种成因机理[J]. 石油勘探与开发,1999, 26(5): 77~79.
22 王振奇,何贞铭,徐龙,赵明跃. 1998. 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,20(2):27~33.
23 Patricia M. Dove. The dissolution kinetics of quartz in sodium chloride solutions at 25°to300°. American Journal of Science,1994,294:665~712.
24 Brady P V. Silica surface chemistry at elevated tempretures. Geochimica et Cosmochimica Acta,1992, 56, 2941～2946.
25 Hiemstra T and van Riemsdija W H. Multiple acticated-complex dissolution of metal(hydr) oxides:A thermodynamic approach applied to quartz. Journal of Colloid and Interface Science,1990,136～ 149.
26 张生,李统锦. 石英溶解动力学研究进展[J]. 世界地质,1996,15(4):8～13.
27 Knauss K G,Wolery T J. The dissolution kinetics of quartz as a function of pH and time at 70°C. Geochim. Cosmochim. Acta,1988,52:43～53.
28 Ronald A.Riley,John Wicks, and John Thomas. Cambrian–Ordovician Knox production in Ohio:Three case studies of structural-stratigraphic traps. AAPG Bulletin,2002,86( 4): 539～555.
29 Wilson M D. Assessing the relative importance of diagenetic processe and controls [A]. In: Wilson M D, ed.Reservoir quality assessment and prediction in clastics rocks[C]. SEPM short Course,1994,30:259~275.
30 田克勤,于志海,冯明,等. 渤海湾盆地下第三系深层油气地质与勘探[M]. 北京:石油工业出版社,2000.
31 谯汉生,方朝亮,牛嘉玉,等. 中国东部深层石油地质[M]. 北京:石油工业出版社,2002.
32 康玉柱. 中国塔里木盆地石油地质特征及资源评价[M]. 北京地质出版社,1996.
33 郭宏莉,应凤祥. 塔里木盆地东河塘地区碎屑岩成岩序列与孔隙演化[J].见:童晓光,梁狄刚,贾承造. 塔里木盆地石油地质研究新进展.北京:科学出版社, 1996.
34 龚再升,李思田,谢泰俊,等. 南海北部大陆边缘盆地分析与油气聚集[M]. 北京:科学出版社,1997.
35 陈纯芳,赵澄林,李会军. 板桥和歧北凹陷沙河街组深层碎屑岩储层物性特征及其影响因素[J].石油大学学报(自然科学版), 2002,26(1):4~7.
36 高勇,张连雪. 板桥—北大港地区深层碎屑岩储集层特征及影响因素研究[J].石油勘探与开发,2001,28(2):36~39.
37 史宏才,朱江庆,王诗中,等. 高温下矿物-水反应的研究[J] .石油学报,1998,19(2):73~80.
38 杨绪充,等. 含油气区地下温压环境[M] .东营:石油大学出版社,1993.
39 Bjorlykee K.,Palme,Mo A. Modelling of thermal convection in sedimentary basins and its relevance to diagenetic reactions,Marine Petroleum. Geol V 5,1988,4:338~351.
40 刘立,于均民,孙晓明,等. 热对流成岩作用的基本特征与研究意义[M].地球科学进展,2000, 15(5):583~585.
41 史基安,王琪. 影响碎屑岩天然气储层物性的主要控制因素[J]. 沉积学报,1995,13(2):128～ 138.
42 Hao Fang,Sun Yongchuan,Li Sitian,et al.. Overpressure re-tardation of organic-matter maturation and petroleum generation:Acasestudy from the Yinggehai and Qiongdongnan Basins, SouthChina Sea.AAPG Bulletin. 1995,79(4):551~562.
43 杨晓宁, 陈洪德, 寿建峰, 张惠良. 碎屑岩次生孔隙形成机制[J]. 大庆石油学院学报,2004,18(1): 4～6.
44 朱国华. 碎屑岩储集层孔隙的形成、演化和预测[J].沉积学报,1992,10(3): 114～123.
45 黄思静, 张萌, 朱世全,等. 砂岩孔隙成因对孔隙度/渗透率关系的控制作用—以鄂尔多斯盆地陇东地区三叠系延长组为例[J]. 成都理工大学学报(自然科学版). 2004,31(6): 648～653.
46 Schmidt, V.& McDonald, D.A. The role of secondary porosity in the course of sandstone diagenesis. In: Aspects of Diagenesis (Eds P.A. Scholle & P.R. Schuldger). Special Publication 29,Society ofEconomic Paleontologists and Mineralogist,Tulsa,OK. 1979: 207~
47 钟大康,朱筱敏,周新源,等. 塔里木盆地中部泥盆系东河砂岩成岩作用与储集性能控制因素[J].古地理学报,2003,5(3):378~390.
48 龚再升,李思田,谢泰俊,等. 南海北部大陆边缘盆地分析与油气聚集[M]. 北京:科学出版社,1997.
49 赵澄林,刘孟彗,纪友亮. 东濮凹陷下第三系碎屑岩沉积体系与成岩作用[M]. 北京:石油工业出版社, 1992.
50 孙永传,李忠,李惠生,等. 中国东部含油气断陷盆地的成岩作用[M]. 北京:科学出版社, 1996.
51 黄思静,谢连文,张 萌,等. 中国三叠系陆相砂岩中自生绿泥石的形成机制及其与储层孔隙保存的关系[J]. 成都理工大学学报(自然科学版),2004,31(3):273~280.
52 Ehrenberg S N. Preservation of anomalously high porosity in deeply buried sandstones by grain-coating chlorite:Examples from the Norwegian Continental Shelf. AAPG Bulletin. 1993, 77:1260~1286.
53 D' A gostino A. Petrography, reservoir qualities , and depositional setting of the Howellsand , deep upper Wilcox, east Seven Sisters field, Dural County, Texas:Gulf Coast Section. Society for Sedimentary Geology Foundation Fourth Annual Research Conference Proceedings. 1985, 243~262.
54 Dixon S A , Summers D M , Surdam R C. Diagenesis and preservation of porosity in Norphlet Formation ( Upper Jurassic ) , southern Alabama. AAPG Bulletin,1989,73:707~728.
55 Dutton S P. Diagenesis and porosity distribution in deltaic sandstone , Strawn series ( Pennsylvanian ) , north–central Texas:Gulf Coast. Association of Geological Societies Transactions. 1977,27: 272~277 .
56 Hancock N J. Possible causes of Rotliegend sandstone diagenesis in northern West Germany. Journal of the Geological Society of London,1978,135:35~ 40.
57 Heald M T,Anderegg R C. Differential cementation in the Tuscarora sandstone. Journal of Sedimentary Petrology,1960,30:568~577.
58 Heald M T, Larese R E. Influence of coatings on quartz cementation. Journal of Sedimentary Petrology,1974,44:1269~1274.
59 Houseknecht DW,Hathon L A. Relationships among thermal maturity, sandstone diagenesis, and reservoir quality in Pennsylvanian strata of the Arkomabasin. AAPGBulletin, 1987,71:568~569.
60 Pittman E D,Lumsden D N. Relationship between chlorite coatings on quartz grains and porosity, Spiro Sand, Oklahoma. Journal of Sedimentary Petrology,1968,38:668~670.
61 Thomson A. Preservation of porosity in the deep Woodbine /Tuscaloosa trend, Louisiana: Gulf Coast. Association of Geological Societies Transactions. 1979,30:396~403.
62 Tillman R W and Almon W R. Diagenesis of the Frontier Formation offshore bar sandstones, Spearhead Ranchfield, Wyoming[J] . SEPM Special Publication,1979,26:337~378.
63 Hurst A, Nadeau H P. Clay microporosity in reservoir sandstones: an application of quantitative electron microscopy in petrophy sical evaluation. AAPG Bulletin,1995,79(4):563~573.
64 Marchand,A.M.E., Smalley, P.C., Haseldine, R.S. et al.. Note on the importance of hudrocarbon fill for reservoir quality prediction in sandstones. American Association of Petroleum Geologists Bulletin,2002,86(9):1561~1571.
65 胡海燕. 油气充注对成岩作用的影响[J]. 海相油气地质,2004,9(1-2):85～90.
66 Lander, R.H. & Walderhaug, O. Reservoir quality prediction through simulation of sandstone compaction and quartz cementation. American Association of Petroleum Geologists Bulletin. 1999,83:433~449.
67 周东升, 刘光祥, 叶军, 贾存善. 深部砂岩异常孔隙的保存机制研究[J]. 石油实验地质, 2004,26(1):40～46.
68 Hoeiland,S.,Barth, A.M. & Skauge, A. The effect of crude oil acid fractions on wettability as studied by interfacial tension and contact angles. Journal of Petroleum Science and Engineering. 2001, 30:91~103.
69 Midtb?,R.E.A.,Rykkje, J.M. & Ramm, M.Deep burial diagenesis and reservoir quality along the eastern flank of the Viking Graben:evidence for illitization and quartz cementation after hydrocarbon emplacement.Clay Minerals. 2000, 35:231~241.
70 郝芳, 邹华耀, 倪建华,等. 沉积盆地超压系统演化与深层油气成藏条件[J]. 地球科学—中国地质大学学报. 2002,27 (5) :610~615.
71 Osborne M J,Swarbrick R E. Diagenesis in North Sea HPHT clastic reservoirs consequences for porosity and overpressure prediction. Marine and Petroleum Geology,1999,16 (4): 337~353.
72 Wilkinson M D, Haszeldine R S, Couples G D.Secondary porosity generation during deep burial associated with overpressure leak off: Fulmar Formation, United Kingdom Central Graben[J ]. A APG B u lletin,1997,81 (5):803~ 813.
73 李会军, 程文艳, 张文才,等. 深层异常温压条件下碎屑岩成岩作用特征初探—以板桥凹陷下第三系深层碎屑岩地层为例[J]. 石油勘探与开发,2001,28 (6): 28~31.
74 Whelan J K, Kennicutt IIM C, Brooks J M,et al. Organic geochemical indications of dynamic fluid flow process in petroleum basins. Organic Geochemistry,1994,22 (3~5):587~ 615.
75 Ghaith A, Chen W, Ortoleva P.Oscillato rymethane release from shale source rock. Earth Science Reviews,1990,29 (1~4):241~248.
76 Roberts S J,Nunn J A. Episodic fluid expulsion from geop ressured sediments. Marine and Petroleum Geology. 1995, 12:195~204.
77 刘林玉,陈刚,柳益群,等. 碎屑岩储集层溶蚀型次生孔隙发育的影响因素分析[J]. 沉积学报. 1998,16 (2): 97~101.
78 林西生,应凤祥,郑乃萱. X 射线衍射分析技术及其地质应用[M]. 北京:石油工业出版社, 1992, 119~131.
79 包书景,何 生. 泌阳凹陷地质流体对砂岩储集层中黏土矿物形成和分布的控制作用[J]. 地质科技情报,2005,24(2): 51~156.
80 于兴河,李剑峰. 油气储层研究所面临的挑战与新动向[J].地学前缘,1995,2(3)、(4):213~219.
81 寿建峰. 碎屑岩储层控制因素及钻前定量地质预测[J].海相油气地质,1999,1:21~26.
82 杨仁超. 储层地质学研究新进展[J].特种油气藏,2006,13(4):: 1~5.
83 杨晓萍,邹才能,李 伟. 四川盆地中部上三叠统香溪群岩性油气藏圈闭类型及其特征[J]. 中国石油勘探,2006,(4):33~36.
84 游章隆,王安发,陈心胜,等. 川东北部香溪群的地震相和有利储层展布[J].成都理工学院学报,1994,21(4):42~50.
85 罗启后,王世谦. 四川盆地中西部三叠系重点含气层系天然气富集条件研究[J].天然气工业,1996,16(增刊):40~54.
86 张金亮,王宝清. 四川盆地中西部上三叠统沉积相[J].西安石油学院学报(自然科学版),2000,15(2):1~6.
87 苟宗海. 四川龙门山中段上三叠统须家河组特征[J].沉积与特提斯地质,2001,21(1):93~101.
88 李耀华,陈更生,张健,等. 川西前陆盆地天然气成藏条件及勘探前景[J].中国石油勘探,2002, 7(1):34~45.
89 董贞环. 四川盆地西部须家河组致密砂岩成岩作用与孔隙演化模式[J].岩相古地理,1994,14(2):33~41.
90 吕正祥. 川西孝泉构造上三叠统超致密储层演化特征[J].成都理工大学学报(自然科学版),2005,32(1):22~26.
91 杜业波,季汉成,朱筱敏. 川西前陆盆地上三叠统须家河组成岩相研究[J].吉林大学学报(地球科学版),2006,36(3):358~364.
92 四川油气区石油地质志编写组. 中国石油地质志.四川卷,北京:石油工业出版社,1990:1~5.
93 郭正吾,韩永辉,等. 四川盆地碎屑岩油气地质图集.四川科学技术出版社,1996:1~14.
94 刘树根,童崇光,罗志立,等. 川西晚三叠系前陆盆地的形成与演化[J].天然气工业,1995, 15(2):11~14.
95 罗志立,龙学明. 龙门山造山带的崛起和川西前陆盆地的沉降[J].四川地质学报, 1992, 12(1):1~17.
96 邓康龄. 四川盆地形成演化与油气勘探领域[J].天然气工业,1992,12(3) .
97 刘树根. 龙门山冲断带与川西前陆盆地的形成演化[M].成都:成都科技大学出版社,1993, 17~64.
98 曾允孚,李勇. 龙门山前陆盆地形成与演化[J]. 矿物岩石,1995,15(1):40~49.
99 何登发,吕修详,等. 前陆盆地分析[M]. 1996,北京,石油工业出版社.
100 刘和甫,梁慧社,等. 川西龙门山冲断系构造样式与前陆盆地演化[J],地质学报,1994,68(2).
101 徐效松,刘宝珺,徐强,等. 中国西部大型盆地分析及地球动力学[M]. 1997,北京:地质出版社.
102 刘树根,童崇光,罗志立,等. 川西晚三叠世前陆盆地的形成与演化[J].天然气工业,1995,15(2):11~14.
103 刘树根,罗志立,曹树恒. 一种新的陆内俯冲类型—龙门山型俯冲成因机制研究.石油实验地质,1991,13(4).
104 Williams G D el al.. Geometry and kinematics of Inversion Tectonics. In:Inversion Tectonic Cedited by M A Cooper and G D Williams, Geo1 Soc Spec Puplication, 1987;(44):3~15.
105 刘树根,罗志立,曹树恒. 四川龙门山冲断带(中北段)岩石圈的层圈性和多级滑脱推覆.四川地质学报,1990,10(3) .
106 侯立伟,等. 藏东川西地区岩浆活动的主要特征及其与板块构造、内生矿产的关系.见:青藏高原地质文集(13),北京:地质出版社,1983,69~106.
107 Conybeare C E B. Litlostratigraphic analysis of sedimentary basins. New York:[S.n.], 1979.
108 李思田. 沉积盆地分析中的沉积体系研究.矿物岩石地球化学通讯,1988,(2).
109 姜在兴. 沉积学[M]. 2003,石油工业出版社.
110 黄其胜. 川北晚三叠世须家河期古气候及成煤特征[J] .地质论评,1995,41(1):92~99.
111 李绍虎,吴冲龙,王华,等. 四川须家河组层序地层格架与天然气成藏的关系[J]. 石油与大然气地质,1998,19(2):146~151.
112 苟宗海. 四川龙门山中段前陆盆地沉积相与层序地层划分[J].沉积与特提斯地质,2000,20(4):79~88.
113 侯方浩,蒋裕强,方少仙,等. 四川盆地上三叠统香溪组二段和四段砂岩沉积模式[J].石油学报,2005,26(2):30~37.
114 庞宏磊,李德敏. 川西坳陷鸭子河构造上三叠统须家河组沉积微相研究[J]. 内蒙古石油化工,2006,(8):132~133.
115 张哨楠. 川西致密砂岩的石英次生加大及其对储层的影响[J]. 地质论评,1998,44(6): 649~655.
116 郑浚茂,应凤祥.煤系地层(酸性水介质)的砂岩储层特征及成岩模式[J].石油学报,1997,
18(4):19～24.
117 Surdam R C, Brosese S W, Crossey L.J. The chemistry of secondary porosity.In:McDonald D A, Surdam R C,eds. Clastic Diagenesis. The American Association of Petroleum Geologists,Tulsa,Oklahoma,1985,127~150.
118 Surdam R C, Grossey L J,Hagen E S, Heasler H P. Organic-inorganic interaction and sandstone diagenesis. AAPG Bulletin,1989,73(1):1~23.
119 谯汉生,方朝亮,牛嘉玉,等. 中国东部深层石油地质[M]. 北京:石油工业出版社,2002.
120 Osborne M J, Swarbrick R E. Diagenesis in North Sea HPHT clastic reservoirs-consequences for porosity and overpressure prediction[J]. Marine and Petroleum Geology, 1999, 16(4):337~353.
121 Wilkinson M D, Haszeldine R S, Couples G D. Secondary porosity generation during deep burial associated with over-pressure leak-off:Fulmar Formation, United Kingdom Central Graben[J]. AAPG Bulletin, 1997, 81(5):803~813.
122 Hunt J M. Generation and migration of petroleum from abnormally pressured fluid compartments[J]. AAPG Bulletin, 1990, 74(1):1~12.
123 Nedkvitne T, BjUrlykke K. Secondary porosity in the Brent Group(MiddleJurassic), Huldar Field,North Sea:Implication for predicting lateral continuity of sandstones[J].Journal of Sedimentary Petrology,1992,62(1):23~34.
124 Sullivan K B, McBride E F. Diagenesis of sandstones at shale contacts and diagenetic heterogeneity, Fris Formation, Texas[J]. AAPG Bulletin, 1991, 75(1):121~138.
125 徐北煤,卢冰. 硅质碎屑岩中碳酸盐胶结物及其对储集层的控制作用研究[J].沉积学报, 1994, 12(3):56～66.
126 庄松生,左燕春,梨琼. 苏北溱潼凹陷戴南组二段成岩作用与次生孔隙预测[J].矿物岩石,1998,18(4):64～71.
127 游俊,郑浚茂. 黄骅坳陷中北区深部储层物性影响因素分析[J].现代地质,1999,13(3):350～ 354.
128 Salman Bloch,Robert H. Lander, and Linda Bonnell.Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Origin and redictability.AAPG Bulletin,2002,86(2):301～
328.
129 Bloch, S..Secondary porosity in sandstones:significance, origin,relationship to subaerial unconformities, and effect on predrill reservoir quality prediction,in M.D.Wilson,ed., Reservoir quality assessment and prediction in clastic rocks: SEPM Short Course,1994, 30, 137～160.
130 Giles, M.R..Diagenesis:a quantitative perspective: Dordrecht, Kluver Academic publishers.1997, 526.
131 Oelkers, E.H., P.A.Bj?rkum, and W. M. Murphy.The mechanism of porosity reduction, stylolite development and quartz cementation in North Sea sandstones, in Y.K.Kharaka and A. S. Maest, eds., Proceedings— International Symposium on Water-Rock Interaction, Rotterdam,Balkema,1992,2:1183～1186.
132 Bj?rkum, P.A., E.H.Oelkers, P.H.Nadeau, O.Walderhaug, and W. M. Murphy.Porosity prediction in quartzose sandstones as a function of time, temperature, depth, stylolite frequency and hydrocarbon saturation:AAPG Bulletin, 1998, 82:637～ 648.
133 Eric H. Oelkers and Harold C.Helgeson. Calculation of dissociation constants and the relative stabilities of polynuclear clusters of 1:1 electrolytes in hydrothermal solutions at supercritical pressures and temperatures. Geochimica et Cosmochimica Acta,1993,57(12):2673～2697.
134 Hiemstra T and van Riemsdija W H. Multiple acticated-complex dissolution of metal(hydr) oxides:A thermodynamic approach applied to quartz.Journal of Colloid and Interface Science, 1990,136～149.
135 J.G.Southwick. Solubilit of silica in Alkaline solutions:Implications for improving flooding. SPE, 1985.
136 Evans,J.Quartz dissolution during shale diagenesis implications for quartz cementation sandstones.Chem Geol,1990,84:NOS 1～4,PP 239～240.
137 Dove P M.Elston S F. The low-temperature dissolution kinetics of quartz in sodium chloride solution:Analysis of exiting data and a rate model for 25°C,pH2～13. Geochimica et Cosmochimica Acta,1992,56:4147～4156.
138 Tester J W,Worley W G , et al.. Correlation quartz dissolution kinetics in pure water from 25 to 625°C.Geochim Cosmochim Acta , 1994,58(11):2407～2420.
139 邱隆伟,姜在兴,操应长,等. 泌阳凹陷碱性成岩作用及其对储层的影响[J].中国科学 D 辑,2001,31(9):752～759.
140 邱隆伟,姜在兴,陈文学,李晓红. 一种新的储层孔隙类型-石英溶解次生孔隙[J].沉积学报,2002,20(4):621～627.
141 陈忠,罗蛰潭,沈明道,等. 由储层矿物在碱性驱替剂中的化学行为到砂岩储层次生孔隙的形成[J].西南石油学院学报,1996,18(2):15～19.
142 罗孝俊,杨卫东,李荣西.pH 值对长石溶解度及次生孔隙发育的影响[J].矿物岩石地球化学通报,2001,20(2):103～107.
143 史丹妮,金巍.砂岩中自生石英的来源、运移与沉淀机制[J].岩相古地理,1999,19(6): 65～70.
144 赵伦,赵澄林,涂强. 酒东盆地营尔凹陷碎屑岩储层成岩作用研究[J].江汉石油学院学报,1998, 20(4):12～16.
145 叶瑛,沈忠悦,郑丽波,等. 塔里木库车坳陷中新生成岩期钠长石化[J].高校地质学报,1999, 5(3):71～79.
146 王允诚,周文,等.川西坳陷上三叠统致密碎屑岩裂缝性气藏分析和储层识别[R].成都理工学院“八五”国家重点科技攻关项目研究成果报告(编号:85-102-07-02-03) .
147 王一刚,余晓锋,杨 雨,等. 流体包裹体在建立四川盆地古地温剖面研究中的应用[J]. 地球科学—中国地质大学学报,1998,23(3):285～288.
148 杨怀辉,李忠惠. 从古热流值和剥蚀量的研究来判断地热的发育-以四川盆地川合 100 井为例[J]. 四川地质学报,2004,24(3):180～184.
149 刘树根,李国蓉,李巨初,等. 川西前陆盆地流体的跨层流动和天燃气爆发式成藏[J].地质学报,2005,79(5):690～699.
150 王世谦,罗启后,邓鸿斌,等. 四川盆地西部侏罗系天然气成藏特征[J].天然气工业,2001, 21(2):1～8.
151 李巨初,刘树根,徐国盛,等.川西前陆盆地流体的跨层流动[J]. 地质地球化学,2001,29(4): 73～81.
152 刘树根,王国芝,徐国盛,等. 龙门山造山带盆山转换时期的流体及流体迁移特征[J].成都理工大学学报(自然科学版),2003,30(1):19～24.
153 J.Hoefs, G. Müller, K. A. Schuster and D.Walde. The Fe-Mn ore deposits of Urucum, Brazil:An oxygen isotope study. Chemical Geology:Isotope Geoscience section,1987,65(3-4):311～ 319.
154 David Mattey,David Lowry and Colin Macpherson.Oxygen isotope composition of mantle peridotite.Earth and Planetary Science Letters,1994,12( 3～4): 231～241.
155 J.L.Harmon, Ph. Duboc and D.Bonvin.Factor analytical modeling of biochemical data.Computers & Chemical Engineering,1995,19(12):1287～1300.
156 上官志冠,白春华,孙明良. 腾冲热海地区现代幔源岩浆气体释放特征[J].中国科学(D)辑,2000, 30(4):407~414.
157 杨晓勇,章雨旭,郑永飞,等. 白云鄂博赋矿白云岩与微晶丘和碳酸岩墙的碳氧同位素对比研究[J].地质学报,2000,74(2):169~180.
158 王先彬,吴茂炳,张铭杰. 地幔流体的稳定同位素地球化学综述[J].地质地球化学,2000,28(3): 69~73.
159 徐国盛,刘树根,李国蓉,等. 川西前陆盆地碎屑岩天然气跨层运移过程中的相态演变[J].成都理工学院学报,2001,28(4):383～388.
160 陈彦华,刘莺. 成岩相-储集体预测的新途径[J]. 石油实验地质,1994,16(3):274～280.
161 钟广法,邬宁芬. 成岩岩相分析:一种全新的成岩非均质性研究方法[J]. 石油勘探与开发,1997,24(5):62～66.
162 王允诚,等. 裂缝性致密油气储集层[M].北京:地质出版社,1992.
163 Oliver J. Fluids expelled tectonically from orogenic belts:Their vole in hydrocarbon migration and other geologic phenomena.Geology,1986,14:99~102.
164 Pilgram C Jet al.. Tectonic controls on Carbonate platform evolution in Southern Papua New Guinea:passive margin to foreland basin. Geology,1989,17:199~202.
2 钱峥,赵澄林,刘孟慧. 济阳坳陷深层天然气致密砂岩储集空间成因[J]. 石油大学学报(自然科学版),1994,18(6):21～25.
3 赵澄林,等.储层沉积学[M]. 北京:石油工业出版社,1998.
4 朱国华,等.成岩作用与砂岩孔隙的演化[M].北京:石油工业出版社,1982.
5 西北大学地质系译. 碎屑岩的成岩作用(译文集)[M]. 西安:西北大学出版社,1986.
6 刘宝珺,张锦泉.沉积成岩作用[ M].北京:科学出版社. 1992, 622,68～92.
7 杨晓宁,陈洪德,寿建峰,等.碎屑岩次生孔隙形成机制[J].大庆石油学院学报, 2004, 28(1) : 4～6.
8 沃尔特·施密特.砂岩成岩过程中地次生储集孔隙[M].北京:石油工业出版社. 1982,272～276.
9 Boles, J.R. Secondary porosity reactions in the Stevens Sandstones, San Joaquin Valley,California. In:Clastic Diagenesis (Eds D.A.McDonald & R.C.Surdam). Memoir 37,American Association of Petroleum Geologists, Tulsa, OK.1984, 217~225.
10 Bj?rlykke,K. Formation of secondary porosity:How important is it? In:Clastic Diagenesis (Eds D.A.McDonald & R.C.Surdam). Memoir 37,American Association of Petroleum Geologists,Tulsa, ok. 1984,277~286.
11 Bloch,S. Secondary porosity in sandstones:Significance,origin,relationship to subaerial unconformities, and effect on predrill reservoir quality prediction. In: Reservoir Quality Assessment and Prediction in Clastic Rocks (Ed.M.D.Wilson). Short Course 30,Society of Sedimentary Geologist,Tulsa,OK. 1994,136~159.
12 黄思静,侯中键.地下孔隙度和渗透率在空间和时间上的变化及影响因素[J].沉积学报. 2001, 19(2) :224～230.
13 朱国华.陕北浊沸石次生孔隙砂体的形成与油气关系[J]. 石油学报. 1985, 6(1) :1～8.
14 寿建峰,朱国华.砂岩储层孔隙保存的定量预测研究[J]. 地质科学. 1998, 32(2) :224～249.
15 邱隆伟,姜在兴.陆源碎屑岩的碱性成岩作用[J]. 地质出版社. 2006, 1～2.
16 Bloch,S.,Lander, R.H. & Bonnell,L. Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Origin and predictability. American Association of Petroleum GeologistsBulletin. 2002,86:301~328.
17 Worden,R.H.& Burley,S.D. Sandstone diagenesis: the evolution of sand to stone. In: Sandstone Diagenesis: Recent and Ancient (Eds S.D.Burley & R.H. Worden). Reprint Series Volume 4 of the International Association of Sedimentologist. Blackwell Science, Oxford. 2003,3~44.
18 裘怿楠, 薛叔浩, 应凤祥. 中国陆相油气储集层[M]. 北京: 石油工业出版社,1997.
19 应凤祥, 罗平, 何东博,等. 中国含油气盆地碎屑岩储集层成岩作用与成岩数值模拟[M]. 北京: 石油工业出版社, 2004.
20 Bloch S. Secondary porosity in sandstones: significance, origion, relationship to subaerial uncomformities, and effect on predrill reservoir quality prediction[A]. in:Wilson M D,ed. Reservoir quality assessment and prediction in clastics rocks[C]. SEPM short Course, 1994, 30: 136~159.
21 陈丽华,赵澄林. 碎屑岩天然气储集层次生孔隙三种成因机理[J]. 石油勘探与开发,1999, 26(5): 77~79.
22 王振奇,何贞铭,徐龙,赵明跃. 1998. 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,20(2):27~33.
23 Patricia M. Dove. The dissolution kinetics of quartz in sodium chloride solutions at 25°to300°. American Journal of Science,1994,294:665~712.
24 Brady P V. Silica surface chemistry at elevated tempretures. Geochimica et Cosmochimica Acta,1992, 56, 2941～2946.
25 Hiemstra T and van Riemsdija W H. Multiple acticated-complex dissolution of metal(hydr) oxides:A thermodynamic approach applied to quartz. Journal of Colloid and Interface Science,1990,136～ 149.
26 张生,李统锦. 石英溶解动力学研究进展[J]. 世界地质,1996,15(4):8～13.
27 Knauss K G,Wolery T J. The dissolution kinetics of quartz as a function of pH and time at 70°C. Geochim. Cosmochim. Acta,1988,52:43～53.
28 Ronald A.Riley,John Wicks, and John Thomas. Cambrian–Ordovician Knox production in Ohio:Three case studies of structural-stratigraphic traps. AAPG Bulletin,2002,86( 4): 539～555.
29 Wilson M D. Assessing the relative importance of diagenetic processe and controls [A]. In: Wilson M D, ed.Reservoir quality assessment and prediction in clastics rocks[C]. SEPM short Course,1994,30:259~275.
30 田克勤,于志海,冯明,等. 渤海湾盆地下第三系深层油气地质与勘探[M]. 北京:石油工业出版社,2000.
31 谯汉生,方朝亮,牛嘉玉,等. 中国东部深层石油地质[M]. 北京:石油工业出版社,2002.
32 康玉柱. 中国塔里木盆地石油地质特征及资源评价[M]. 北京地质出版社,1996.
33 郭宏莉,应凤祥. 塔里木盆地东河塘地区碎屑岩成岩序列与孔隙演化[J].见:童晓光,梁狄刚,贾承造. 塔里木盆地石油地质研究新进展.北京:科学出版社, 1996.
34 龚再升,李思田,谢泰俊,等. 南海北部大陆边缘盆地分析与油气聚集[M]. 北京:科学出版社,1997.
35 陈纯芳,赵澄林,李会军. 板桥和歧北凹陷沙河街组深层碎屑岩储层物性特征及其影响因素[J].石油大学学报(自然科学版), 2002,26(1):4~7.
36 高勇,张连雪. 板桥—北大港地区深层碎屑岩储集层特征及影响因素研究[J].石油勘探与开发,2001,28(2):36~39.
37 史宏才,朱江庆,王诗中,等. 高温下矿物-水反应的研究[J] .石油学报,1998,19(2):73~80.
38 杨绪充,等. 含油气区地下温压环境[M] .东营:石油大学出版社,1993.
39 Bjorlykee K.,Palme,Mo A. Modelling of thermal convection in sedimentary basins and its relevance to diagenetic reactions,Marine Petroleum. Geol V 5,1988,4:338~351.
40 刘立,于均民,孙晓明,等. 热对流成岩作用的基本特征与研究意义[M].地球科学进展,2000, 15(5):583~585.
41 史基安,王琪. 影响碎屑岩天然气储层物性的主要控制因素[J]. 沉积学报,1995,13(2):128～ 138.
42 Hao Fang,Sun Yongchuan,Li Sitian,et al.. Overpressure re-tardation of organic-matter maturation and petroleum generation:Acasestudy from the Yinggehai and Qiongdongnan Basins, SouthChina Sea.AAPG Bulletin. 1995,79(4):551~562.
43 杨晓宁, 陈洪德, 寿建峰, 张惠良. 碎屑岩次生孔隙形成机制[J]. 大庆石油学院学报,2004,18(1): 4～6.
44 朱国华. 碎屑岩储集层孔隙的形成、演化和预测[J].沉积学报,1992,10(3): 114～123.
45 黄思静, 张萌, 朱世全,等. 砂岩孔隙成因对孔隙度/渗透率关系的控制作用—以鄂尔多斯盆地陇东地区三叠系延长组为例[J]. 成都理工大学学报(自然科学版). 2004,31(6): 648～653.
46 Schmidt, V.& McDonald, D.A. The role of secondary porosity in the course of sandstone diagenesis. In: Aspects of Diagenesis (Eds P.A. Scholle & P.R. Schuldger). Special Publication 29,Society ofEconomic Paleontologists and Mineralogist,Tulsa,OK. 1979: 207~
47 钟大康,朱筱敏,周新源,等. 塔里木盆地中部泥盆系东河砂岩成岩作用与储集性能控制因素[J].古地理学报,2003,5(3):378~390.
48 龚再升,李思田,谢泰俊,等. 南海北部大陆边缘盆地分析与油气聚集[M]. 北京:科学出版社,1997.
49 赵澄林,刘孟彗,纪友亮. 东濮凹陷下第三系碎屑岩沉积体系与成岩作用[M]. 北京:石油工业出版社, 1992.
50 孙永传,李忠,李惠生,等. 中国东部含油气断陷盆地的成岩作用[M]. 北京:科学出版社, 1996.
51 黄思静,谢连文,张 萌,等. 中国三叠系陆相砂岩中自生绿泥石的形成机制及其与储层孔隙保存的关系[J]. 成都理工大学学报(自然科学版),2004,31(3):273~280.
52 Ehrenberg S N. Preservation of anomalously high porosity in deeply buried sandstones by grain-coating chlorite:Examples from the Norwegian Continental Shelf. AAPG Bulletin. 1993, 77:1260~1286.
53 D' A gostino A. Petrography, reservoir qualities , and depositional setting of the Howellsand , deep upper Wilcox, east Seven Sisters field, Dural County, Texas:Gulf Coast Section. Society for Sedimentary Geology Foundation Fourth Annual Research Conference Proceedings. 1985, 243~262.
54 Dixon S A , Summers D M , Surdam R C. Diagenesis and preservation of porosity in Norphlet Formation ( Upper Jurassic ) , southern Alabama. AAPG Bulletin,1989,73:707~728.
55 Dutton S P. Diagenesis and porosity distribution in deltaic sandstone , Strawn series ( Pennsylvanian ) , north–central Texas:Gulf Coast. Association of Geological Societies Transactions. 1977,27: 272~277 .
56 Hancock N J. Possible causes of Rotliegend sandstone diagenesis in northern West Germany. Journal of the Geological Society of London,1978,135:35~ 40.
57 Heald M T,Anderegg R C. Differential cementation in the Tuscarora sandstone. Journal of Sedimentary Petrology,1960,30:568~577.
58 Heald M T, Larese R E. Influence of coatings on quartz cementation. Journal of Sedimentary Petrology,1974,44:1269~1274.
59 Houseknecht DW,Hathon L A. Relationships among thermal maturity, sandstone diagenesis, and reservoir quality in Pennsylvanian strata of the Arkomabasin. AAPGBulletin, 1987,71:568~569.
60 Pittman E D,Lumsden D N. Relationship between chlorite coatings on quartz grains and porosity, Spiro Sand, Oklahoma. Journal of Sedimentary Petrology,1968,38:668~670.
61 Thomson A. Preservation of porosity in the deep Woodbine /Tuscaloosa trend, Louisiana: Gulf Coast. Association of Geological Societies Transactions. 1979,30:396~403.
62 Tillman R W and Almon W R. Diagenesis of the Frontier Formation offshore bar sandstones, Spearhead Ranchfield, Wyoming[J] . SEPM Special Publication,1979,26:337~378.
63 Hurst A, Nadeau H P. Clay microporosity in reservoir sandstones: an application of quantitative electron microscopy in petrophy sical evaluation. AAPG Bulletin,1995,79(4):563~573.
64 Marchand,A.M.E., Smalley, P.C., Haseldine, R.S. et al.. Note on the importance of hudrocarbon fill for reservoir quality prediction in sandstones. American Association of Petroleum Geologists Bulletin,2002,86(9):1561~1571.
65 胡海燕. 油气充注对成岩作用的影响[J]. 海相油气地质,2004,9(1-2):85～90.
66 Lander, R.H. & Walderhaug, O. Reservoir quality prediction through simulation of sandstone compaction and quartz cementation. American Association of Petroleum Geologists Bulletin. 1999,83:433~449.
67 周东升, 刘光祥, 叶军, 贾存善. 深部砂岩异常孔隙的保存机制研究[J]. 石油实验地质, 2004,26(1):40～46.
68 Hoeiland,S.,Barth, A.M. & Skauge, A. The effect of crude oil acid fractions on wettability as studied by interfacial tension and contact angles. Journal of Petroleum Science and Engineering. 2001, 30:91~103.
69 Midtb?,R.E.A.,Rykkje, J.M. & Ramm, M.Deep burial diagenesis and reservoir quality along the eastern flank of the Viking Graben:evidence for illitization and quartz cementation after hydrocarbon emplacement.Clay Minerals. 2000, 35:231~241.
70 郝芳, 邹华耀, 倪建华,等. 沉积盆地超压系统演化与深层油气成藏条件[J]. 地球科学—中国地质大学学报. 2002,27 (5) :610~615.
71 Osborne M J,Swarbrick R E. Diagenesis in North Sea HPHT clastic reservoirs consequences for porosity and overpressure prediction. Marine and Petroleum Geology,1999,16 (4): 337~353.
72 Wilkinson M D, Haszeldine R S, Couples G D.Secondary porosity generation during deep burial associated with overpressure leak off: Fulmar Formation, United Kingdom Central Graben[J ]. A APG B u lletin,1997,81 (5):803~ 813.
73 李会军, 程文艳, 张文才,等. 深层异常温压条件下碎屑岩成岩作用特征初探—以板桥凹陷下第三系深层碎屑岩地层为例[J]. 石油勘探与开发,2001,28 (6): 28~31.
74 Whelan J K, Kennicutt IIM C, Brooks J M,et al. Organic geochemical indications of dynamic fluid flow process in petroleum basins. Organic Geochemistry,1994,22 (3~5):587~ 615.
75 Ghaith A, Chen W, Ortoleva P.Oscillato rymethane release from shale source rock. Earth Science Reviews,1990,29 (1~4):241~248.
76 Roberts S J,Nunn J A. Episodic fluid expulsion from geop ressured sediments. Marine and Petroleum Geology. 1995, 12:195~204.
77 刘林玉,陈刚,柳益群,等. 碎屑岩储集层溶蚀型次生孔隙发育的影响因素分析[J]. 沉积学报. 1998,16 (2): 97~101.
78 林西生,应凤祥,郑乃萱. X 射线衍射分析技术及其地质应用[M]. 北京:石油工业出版社, 1992, 119~131.
79 包书景,何 生. 泌阳凹陷地质流体对砂岩储集层中黏土矿物形成和分布的控制作用[J]. 地质科技情报,2005,24(2): 51~156.
80 于兴河,李剑峰. 油气储层研究所面临的挑战与新动向[J].地学前缘,1995,2(3)、(4):213~219.
81 寿建峰. 碎屑岩储层控制因素及钻前定量地质预测[J].海相油气地质,1999,1:21~26.
82 杨仁超. 储层地质学研究新进展[J].特种油气藏,2006,13(4):: 1~5.
83 杨晓萍,邹才能,李 伟. 四川盆地中部上三叠统香溪群岩性油气藏圈闭类型及其特征[J]. 中国石油勘探,2006,(4):33~36.
84 游章隆,王安发,陈心胜,等. 川东北部香溪群的地震相和有利储层展布[J].成都理工学院学报,1994,21(4):42~50.
85 罗启后,王世谦. 四川盆地中西部三叠系重点含气层系天然气富集条件研究[J].天然气工业,1996,16(增刊):40~54.
86 张金亮,王宝清. 四川盆地中西部上三叠统沉积相[J].西安石油学院学报(自然科学版),2000,15(2):1~6.
87 苟宗海. 四川龙门山中段上三叠统须家河组特征[J].沉积与特提斯地质,2001,21(1):93~101.
88 李耀华,陈更生,张健,等. 川西前陆盆地天然气成藏条件及勘探前景[J].中国石油勘探,2002, 7(1):34~45.
89 董贞环. 四川盆地西部须家河组致密砂岩成岩作用与孔隙演化模式[J].岩相古地理,1994,14(2):33~41.
90 吕正祥. 川西孝泉构造上三叠统超致密储层演化特征[J].成都理工大学学报(自然科学版),2005,32(1):22~26.
91 杜业波,季汉成,朱筱敏. 川西前陆盆地上三叠统须家河组成岩相研究[J].吉林大学学报(地球科学版),2006,36(3):358~364.
92 四川油气区石油地质志编写组. 中国石油地质志.四川卷,北京:石油工业出版社,1990:1~5.
93 郭正吾,韩永辉,等. 四川盆地碎屑岩油气地质图集.四川科学技术出版社,1996:1~14.
94 刘树根,童崇光,罗志立,等. 川西晚三叠系前陆盆地的形成与演化[J].天然气工业,1995, 15(2):11~14.
95 罗志立,龙学明. 龙门山造山带的崛起和川西前陆盆地的沉降[J].四川地质学报, 1992, 12(1):1~17.
96 邓康龄. 四川盆地形成演化与油气勘探领域[J].天然气工业,1992,12(3) .
97 刘树根. 龙门山冲断带与川西前陆盆地的形成演化[M].成都:成都科技大学出版社,1993, 17~64.
98 曾允孚,李勇. 龙门山前陆盆地形成与演化[J]. 矿物岩石,1995,15(1):40~49.
99 何登发,吕修详,等. 前陆盆地分析[M]. 1996,北京,石油工业出版社.
100 刘和甫,梁慧社,等. 川西龙门山冲断系构造样式与前陆盆地演化[J],地质学报,1994,68(2).
101 徐效松,刘宝珺,徐强,等. 中国西部大型盆地分析及地球动力学[M]. 1997,北京:地质出版社.
102 刘树根,童崇光,罗志立,等. 川西晚三叠世前陆盆地的形成与演化[J].天然气工业,1995,15(2):11~14.
103 刘树根,罗志立,曹树恒. 一种新的陆内俯冲类型—龙门山型俯冲成因机制研究.石油实验地质,1991,13(4).
104 Williams G D el al.. Geometry and kinematics of Inversion Tectonics. In:Inversion Tectonic Cedited by M A Cooper and G D Williams, Geo1 Soc Spec Puplication, 1987;(44):3~15.
105 刘树根,罗志立,曹树恒. 四川龙门山冲断带(中北段)岩石圈的层圈性和多级滑脱推覆.四川地质学报,1990,10(3) .
106 侯立伟,等. 藏东川西地区岩浆活动的主要特征及其与板块构造、内生矿产的关系.见:青藏高原地质文集(13),北京:地质出版社,1983,69~106.
107 Conybeare C E B. Litlostratigraphic analysis of sedimentary basins. New York:[S.n.], 1979.
108 李思田. 沉积盆地分析中的沉积体系研究.矿物岩石地球化学通讯,1988,(2).
109 姜在兴. 沉积学[M]. 2003,石油工业出版社.
110 黄其胜. 川北晚三叠世须家河期古气候及成煤特征[J] .地质论评,1995,41(1):92~99.
111 李绍虎,吴冲龙,王华,等. 四川须家河组层序地层格架与天然气成藏的关系[J]. 石油与大然气地质,1998,19(2):146~151.
112 苟宗海. 四川龙门山中段前陆盆地沉积相与层序地层划分[J].沉积与特提斯地质,2000,20(4):79~88.
113 侯方浩,蒋裕强,方少仙,等. 四川盆地上三叠统香溪组二段和四段砂岩沉积模式[J].石油学报,2005,26(2):30~37.
114 庞宏磊,李德敏. 川西坳陷鸭子河构造上三叠统须家河组沉积微相研究[J]. 内蒙古石油化工,2006,(8):132~133.
115 张哨楠. 川西致密砂岩的石英次生加大及其对储层的影响[J]. 地质论评,1998,44(6): 649~655.
116 郑浚茂,应凤祥.煤系地层(酸性水介质)的砂岩储层特征及成岩模式[J].石油学报,1997,
18(4):19～24.
117 Surdam R C, Brosese S W, Crossey L.J. The chemistry of secondary porosity.In:McDonald D A, Surdam R C,eds. Clastic Diagenesis. The American Association of Petroleum Geologists,Tulsa,Oklahoma,1985,127~150.
118 Surdam R C, Grossey L J,Hagen E S, Heasler H P. Organic-inorganic interaction and sandstone diagenesis. AAPG Bulletin,1989,73(1):1~23.
119 谯汉生,方朝亮,牛嘉玉,等. 中国东部深层石油地质[M]. 北京:石油工业出版社,2002.
120 Osborne M J, Swarbrick R E. Diagenesis in North Sea HPHT clastic reservoirs-consequences for porosity and overpressure prediction[J]. Marine and Petroleum Geology, 1999, 16(4):337~353.
121 Wilkinson M D, Haszeldine R S, Couples G D. Secondary porosity generation during deep burial associated with over-pressure leak-off:Fulmar Formation, United Kingdom Central Graben[J]. AAPG Bulletin, 1997, 81(5):803~813.
122 Hunt J M. Generation and migration of petroleum from abnormally pressured fluid compartments[J]. AAPG Bulletin, 1990, 74(1):1~12.
123 Nedkvitne T, BjUrlykke K. Secondary porosity in the Brent Group(MiddleJurassic), Huldar Field,North Sea:Implication for predicting lateral continuity of sandstones[J].Journal of Sedimentary Petrology,1992,62(1):23~34.
124 Sullivan K B, McBride E F. Diagenesis of sandstones at shale contacts and diagenetic heterogeneity, Fris Formation, Texas[J]. AAPG Bulletin, 1991, 75(1):121~138.
125 徐北煤,卢冰. 硅质碎屑岩中碳酸盐胶结物及其对储集层的控制作用研究[J].沉积学报, 1994, 12(3):56～66.
126 庄松生,左燕春,梨琼. 苏北溱潼凹陷戴南组二段成岩作用与次生孔隙预测[J].矿物岩石,1998,18(4):64～71.
127 游俊,郑浚茂. 黄骅坳陷中北区深部储层物性影响因素分析[J].现代地质,1999,13(3):350～ 354.
128 Salman Bloch,Robert H. Lander, and Linda Bonnell.Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Origin and redictability.AAPG Bulletin,2002,86(2):301～
328.
129 Bloch, S..Secondary porosity in sandstones:significance, origin,relationship to subaerial unconformities, and effect on predrill reservoir quality prediction,in M.D.Wilson,ed., Reservoir quality assessment and prediction in clastic rocks: SEPM Short Course,1994, 30, 137～160.
130 Giles, M.R..Diagenesis:a quantitative perspective: Dordrecht, Kluver Academic publishers.1997, 526.
131 Oelkers, E.H., P.A.Bj?rkum, and W. M. Murphy.The mechanism of porosity reduction, stylolite development and quartz cementation in North Sea sandstones, in Y.K.Kharaka and A. S. Maest, eds., Proceedings— International Symposium on Water-Rock Interaction, Rotterdam,Balkema,1992,2:1183～1186.
132 Bj?rkum, P.A., E.H.Oelkers, P.H.Nadeau, O.Walderhaug, and W. M. Murphy.Porosity prediction in quartzose sandstones as a function of time, temperature, depth, stylolite frequency and hydrocarbon saturation:AAPG Bulletin, 1998, 82:637～ 648.
133 Eric H. Oelkers and Harold C.Helgeson. Calculation of dissociation constants and the relative stabilities of polynuclear clusters of 1:1 electrolytes in hydrothermal solutions at supercritical pressures and temperatures. Geochimica et Cosmochimica Acta,1993,57(12):2673～2697.
134 Hiemstra T and van Riemsdija W H. Multiple acticated-complex dissolution of metal(hydr) oxides:A thermodynamic approach applied to quartz.Journal of Colloid and Interface Science, 1990,136～149.
135 J.G.Southwick. Solubilit of silica in Alkaline solutions:Implications for improving flooding. SPE, 1985.
136 Evans,J.Quartz dissolution during shale diagenesis implications for quartz cementation sandstones.Chem Geol,1990,84:NOS 1～4,PP 239～240.
137 Dove P M.Elston S F. The low-temperature dissolution kinetics of quartz in sodium chloride solution:Analysis of exiting data and a rate model for 25°C,pH2～13. Geochimica et Cosmochimica Acta,1992,56:4147～4156.
138 Tester J W,Worley W G , et al.. Correlation quartz dissolution kinetics in pure water from 25 to 625°C.Geochim Cosmochim Acta , 1994,58(11):2407～2420.
139 邱隆伟,姜在兴,操应长,等. 泌阳凹陷碱性成岩作用及其对储层的影响[J].中国科学 D 辑,2001,31(9):752～759.
140 邱隆伟,姜在兴,陈文学,李晓红. 一种新的储层孔隙类型-石英溶解次生孔隙[J].沉积学报,2002,20(4):621～627.
141 陈忠,罗蛰潭,沈明道,等. 由储层矿物在碱性驱替剂中的化学行为到砂岩储层次生孔隙的形成[J].西南石油学院学报,1996,18(2):15～19.
142 罗孝俊,杨卫东,李荣西.pH 值对长石溶解度及次生孔隙发育的影响[J].矿物岩石地球化学通报,2001,20(2):103～107.
143 史丹妮,金巍.砂岩中自生石英的来源、运移与沉淀机制[J].岩相古地理,1999,19(6): 65～70.
144 赵伦,赵澄林,涂强. 酒东盆地营尔凹陷碎屑岩储层成岩作用研究[J].江汉石油学院学报,1998, 20(4):12～16.
145 叶瑛,沈忠悦,郑丽波,等. 塔里木库车坳陷中新生成岩期钠长石化[J].高校地质学报,1999, 5(3):71～79.
146 王允诚,周文,等.川西坳陷上三叠统致密碎屑岩裂缝性气藏分析和储层识别[R].成都理工学院“八五”国家重点科技攻关项目研究成果报告(编号:85-102-07-02-03) .
147 王一刚,余晓锋,杨 雨,等. 流体包裹体在建立四川盆地古地温剖面研究中的应用[J]. 地球科学—中国地质大学学报,1998,23(3):285～288.
148 杨怀辉,李忠惠. 从古热流值和剥蚀量的研究来判断地热的发育-以四川盆地川合 100 井为例[J]. 四川地质学报,2004,24(3):180～184.
149 刘树根,李国蓉,李巨初,等. 川西前陆盆地流体的跨层流动和天燃气爆发式成藏[J].地质学报,2005,79(5):690～699.
150 王世谦,罗启后,邓鸿斌,等. 四川盆地西部侏罗系天然气成藏特征[J].天然气工业,2001, 21(2):1～8.
151 李巨初,刘树根,徐国盛,等.川西前陆盆地流体的跨层流动[J]. 地质地球化学,2001,29(4): 73～81.
152 刘树根,王国芝,徐国盛,等. 龙门山造山带盆山转换时期的流体及流体迁移特征[J].成都理工大学学报(自然科学版),2003,30(1):19～24.
153 J.Hoefs, G. Müller, K. A. Schuster and D.Walde. The Fe-Mn ore deposits of Urucum, Brazil:An oxygen isotope study. Chemical Geology:Isotope Geoscience section,1987,65(3-4):311～ 319.
154 David Mattey,David Lowry and Colin Macpherson.Oxygen isotope composition of mantle peridotite.Earth and Planetary Science Letters,1994,12( 3～4): 231～241.
155 J.L.Harmon, Ph. Duboc and D.Bonvin.Factor analytical modeling of biochemical data.Computers & Chemical Engineering,1995,19(12):1287～1300.
156 上官志冠,白春华,孙明良. 腾冲热海地区现代幔源岩浆气体释放特征[J].中国科学(D)辑,2000, 30(4):407~414.
157 杨晓勇,章雨旭,郑永飞,等. 白云鄂博赋矿白云岩与微晶丘和碳酸岩墙的碳氧同位素对比研究[J].地质学报,2000,74(2):169~180.
158 王先彬,吴茂炳,张铭杰. 地幔流体的稳定同位素地球化学综述[J].地质地球化学,2000,28(3): 69~73.
159 徐国盛,刘树根,李国蓉,等. 川西前陆盆地碎屑岩天然气跨层运移过程中的相态演变[J].成都理工学院学报,2001,28(4):383～388.
160 陈彦华,刘莺. 成岩相-储集体预测的新途径[J]. 石油实验地质,1994,16(3):274～280.
161 钟广法,邬宁芬. 成岩岩相分析:一种全新的成岩非均质性研究方法[J]. 石油勘探与开发,1997,24(5):62～66.
162 王允诚,等. 裂缝性致密油气储集层[M].北京:地质出版社,1992.
163 Oliver J. Fluids expelled tectonically from orogenic belts:Their vole in hydrocarbon migration and other geologic phenomena.Geology,1986,14:99~102.
164 Pilgram C Jet al.. Tectonic controls on Carbonate platform evolution in Southern Papua New Guinea:passive margin to foreland basin. Geology,1989,17:199~202.