渤南—孤北地区深层天然气成藏机理研究
|
摘要
在国内外典型深层天然气藏成藏特征调研基础上,运用天然气成藏理论,综合运用各种基础资料,应用盆地模拟、流体包裹体分析、储层沥青分析等技术方法,对渤南-孤北地区的深层天然气成藏时间、输导体系、天然气成因判别、成藏动态过程等进行了系统分析。
通过气源岩生烃史、包裹体均一温度、天然气轻烃及构造活动综合分析,明确了渤南-孤北地区深层天然气藏的形成时间和期次。研究表明,孤北潜山带存在两期不同成因天然气的充注过程:煤成气于馆陶组沉积中期充注,油型气于明化镇组沉积初期充注。渤南洼陷油型气藏存在沙一段沉积末期到东营末期和馆陶组沉积初期至今的两次充注过程,以明化镇组沉积时期至今的充注为主。成藏期受构造控制明显,构造低部位气藏形成时间早于高部位。
从地质背景出发,在输导要素(断层、砂体、裂缝等)分布特征和输导机理研究的基础上,根据天然气地化资料、地层水矿化度、断层输导效率、储层沥青、生标物的变化特征等综合分析,认为不同地区、不同成因天然气的输导体系类型存在差异:渤南洼陷裂解气和孤北潜山带的煤成气主要以砂体输导为主,煤成气运移方向受构造形态控制;断阶带裂解气以断层输导为主,且同一断层不同部位输导效率存在差异。天然气成因类型判识表明,研究区存在多种来源、多种成因的天然气:孤北潜山带以石炭-二叠系煤成气为主;渤深4断阶带为油型干酪根裂解气;渤南深洼带和渤深6潜山带为原油裂解气。结合流体包裹体GOI分析表明,孤北古1井古气水界面在现今气水界面之上,表明气藏为多期充注的结果,且后期的充注量较大,保存条件较好。
根据深层天然气成藏机理分析,建立了渤南地区“单源多成因多期成藏模式”和孤北地区“多源多成因多期成藏模式”。渤南地区深层气藏主要来源于同一气源即洼陷区沙四上亚段,其成因包括干酪根裂解气和原油裂解气两类,并且存在沙一末-东营末期和馆陶组沉积初期的两次充注过程;孤北地区深层气藏主要为渤南洼陷沙四上亚段的裂解气和孤北潜山带石炭-二叠系煤成气的混合成藏,以不同成因天然气的多期成藏为主,明化镇组沉积时期充注量最大。
On the basis of the documentary research on the reservoir-forming characteristics of the typical deep gas reservoirs all around the world, applying theories on Gas reservoir-forming, and the combination of various radical informations, lots of techniques, such as basin modelling, high accuracy fluid inclusion testing and analysis, reservoir bitumen analysis, are fully used to analyse the reservoir-forming characteristics of Bonan-Gubei area, Jiyang Depression, including the reservoir’s formation period, hydrocarbon migration pathway, the distinguishment of the gas genetic model and the dynamic procedure of reservoir forming.
Here in this paper, the formation time and stage of the deep gas reservoir are ascertained by a set of analysis techniques, including the hydrocarbon generation history, fluid inclusion homogenization temperature testing, light hydrocarbon characteristic and structure movement analysis. Subsequently, two periods of different original gas chargements consisting of coal-formed gas chargements in middle stage of Ng and oil-formed gas chargements in early stage of Nm in Gubei buried hill belt are established. At the same time, there are two accumulation periods which include from late stage of Es1 to late stage of Ed and from early stage of Ng to nowadays in oil-associated gas reservoirs in Bonan sub-sag, the accumulation of late stage of Nm plays important part, and the accumulative phase is dominated by structure apparently, the fomation period of gas reservoir at downstructure location is earlier than that of gas pool at upstructure location.
From the geological setting, after studying the pattern and mechanism of migration factors which include sand bodies, faults, fractures and so on, according to the alteration characteristic of the geochemical datas of natural gas, degree of mineralization of formation water, reservoir bitumen, the fault effeciency and the biomarkers in the migration pathways, it can be easily to obtain the recognition that gas migration system categories with different genetic mechanisms and in different areas are different: cracked gas in Bonan sub-sag and coal-formed gas in GuBei buried hill migrate along sand bodies mostly, and the migration direction of the latter is dependent on structural attitude. Cracked gas in the block belt travels along the fault chiefly. In addition, the migration effectiveness in different sections of a fault is different.
The origin identification of natural gas demonstrates that the region of interest has multiple sources and different origin types of gas: coal-cracked gas from Carboniferous-Permian source rocks migrates into the trap in Gubei buried hill, kerogen-cracked gas mainly appears in Boshen 4 fault blocks; and whereas oil-cracked gas dominates in deep-zone of Bonan sub-sag and Boshen 6 buried hill zone. Associated with high accuracy fluid inclusion testing and the analysis of GOI, it may be easy to get the conclusion that the palo-gas/water contact is above the present gas/water contact in well Gbg-1, which may indicate a combination of different types of gas accumulation and an increasement in the gas migration quantity in later stage,along with favourable preservation.
On the foundation of deep natral gas reservoir-forming mechanism, two types of reservoir formation pattern are established respectively: one source, muti-types and polyphase reservoir-forming pattern in Bonan area and muti-sources, muti-types and polyphase reservoir -forming pattern in GuBei area. The gas making up the deep gas reservoir in Bonan sub-sag almost comes from the same source rocks in Es4s, which consists of kerogen-cracked and oil-cracked gas, and with twice chargement periods including from late stage of Es1 to late stage of Ed and from early stage of Ng to nowadays. At the same time, the deep gas reservoir in Gubei aera is composed of the gas from Es4s source rocks in Bonan sub-sag and Carboniferous-Permian gas source rocks in Gubei buried hill zone, and it has the character of different types of gas migrating into the trap at different periods, while the chargement dimention reaches maxinum in late stage of Nm.
通过气源岩生烃史、包裹体均一温度、天然气轻烃及构造活动综合分析,明确了渤南-孤北地区深层天然气藏的形成时间和期次。研究表明,孤北潜山带存在两期不同成因天然气的充注过程:煤成气于馆陶组沉积中期充注,油型气于明化镇组沉积初期充注。渤南洼陷油型气藏存在沙一段沉积末期到东营末期和馆陶组沉积初期至今的两次充注过程,以明化镇组沉积时期至今的充注为主。成藏期受构造控制明显,构造低部位气藏形成时间早于高部位。
从地质背景出发,在输导要素(断层、砂体、裂缝等)分布特征和输导机理研究的基础上,根据天然气地化资料、地层水矿化度、断层输导效率、储层沥青、生标物的变化特征等综合分析,认为不同地区、不同成因天然气的输导体系类型存在差异:渤南洼陷裂解气和孤北潜山带的煤成气主要以砂体输导为主,煤成气运移方向受构造形态控制;断阶带裂解气以断层输导为主,且同一断层不同部位输导效率存在差异。天然气成因类型判识表明,研究区存在多种来源、多种成因的天然气:孤北潜山带以石炭-二叠系煤成气为主;渤深4断阶带为油型干酪根裂解气;渤南深洼带和渤深6潜山带为原油裂解气。结合流体包裹体GOI分析表明,孤北古1井古气水界面在现今气水界面之上,表明气藏为多期充注的结果,且后期的充注量较大,保存条件较好。
根据深层天然气成藏机理分析,建立了渤南地区“单源多成因多期成藏模式”和孤北地区“多源多成因多期成藏模式”。渤南地区深层气藏主要来源于同一气源即洼陷区沙四上亚段,其成因包括干酪根裂解气和原油裂解气两类,并且存在沙一末-东营末期和馆陶组沉积初期的两次充注过程;孤北地区深层气藏主要为渤南洼陷沙四上亚段的裂解气和孤北潜山带石炭-二叠系煤成气的混合成藏,以不同成因天然气的多期成藏为主,明化镇组沉积时期充注量最大。
On the basis of the documentary research on the reservoir-forming characteristics of the typical deep gas reservoirs all around the world, applying theories on Gas reservoir-forming, and the combination of various radical informations, lots of techniques, such as basin modelling, high accuracy fluid inclusion testing and analysis, reservoir bitumen analysis, are fully used to analyse the reservoir-forming characteristics of Bonan-Gubei area, Jiyang Depression, including the reservoir’s formation period, hydrocarbon migration pathway, the distinguishment of the gas genetic model and the dynamic procedure of reservoir forming.
Here in this paper, the formation time and stage of the deep gas reservoir are ascertained by a set of analysis techniques, including the hydrocarbon generation history, fluid inclusion homogenization temperature testing, light hydrocarbon characteristic and structure movement analysis. Subsequently, two periods of different original gas chargements consisting of coal-formed gas chargements in middle stage of Ng and oil-formed gas chargements in early stage of Nm in Gubei buried hill belt are established. At the same time, there are two accumulation periods which include from late stage of Es1 to late stage of Ed and from early stage of Ng to nowadays in oil-associated gas reservoirs in Bonan sub-sag, the accumulation of late stage of Nm plays important part, and the accumulative phase is dominated by structure apparently, the fomation period of gas reservoir at downstructure location is earlier than that of gas pool at upstructure location.
From the geological setting, after studying the pattern and mechanism of migration factors which include sand bodies, faults, fractures and so on, according to the alteration characteristic of the geochemical datas of natural gas, degree of mineralization of formation water, reservoir bitumen, the fault effeciency and the biomarkers in the migration pathways, it can be easily to obtain the recognition that gas migration system categories with different genetic mechanisms and in different areas are different: cracked gas in Bonan sub-sag and coal-formed gas in GuBei buried hill migrate along sand bodies mostly, and the migration direction of the latter is dependent on structural attitude. Cracked gas in the block belt travels along the fault chiefly. In addition, the migration effectiveness in different sections of a fault is different.
The origin identification of natural gas demonstrates that the region of interest has multiple sources and different origin types of gas: coal-cracked gas from Carboniferous-Permian source rocks migrates into the trap in Gubei buried hill, kerogen-cracked gas mainly appears in Boshen 4 fault blocks; and whereas oil-cracked gas dominates in deep-zone of Bonan sub-sag and Boshen 6 buried hill zone. Associated with high accuracy fluid inclusion testing and the analysis of GOI, it may be easy to get the conclusion that the palo-gas/water contact is above the present gas/water contact in well Gbg-1, which may indicate a combination of different types of gas accumulation and an increasement in the gas migration quantity in later stage,along with favourable preservation.
On the foundation of deep natral gas reservoir-forming mechanism, two types of reservoir formation pattern are established respectively: one source, muti-types and polyphase reservoir-forming pattern in Bonan area and muti-sources, muti-types and polyphase reservoir -forming pattern in GuBei area. The gas making up the deep gas reservoir in Bonan sub-sag almost comes from the same source rocks in Es4s, which consists of kerogen-cracked and oil-cracked gas, and with twice chargement periods including from late stage of Es1 to late stage of Ed and from early stage of Ng to nowadays. At the same time, the deep gas reservoir in Gubei aera is composed of the gas from Es4s source rocks in Bonan sub-sag and Carboniferous-Permian gas source rocks in Gubei buried hill zone, and it has the character of different types of gas migrating into the trap at different periods, while the chargement dimention reaches maxinum in late stage of Nm.
引文
[1]史斗,刘文汇,郑军卫.深层气理论分析和深层气潜势研究[J].地球科学进展,2003, 18(2):236-243
[2]张义纲著.天然气的生成聚集与保存[M].南京:河海大学出版社,1991,49-157
[3]蒋有录,张一伟.天然气藏与油藏形成机理及分布特征的异同[J].地质科技情报,2000,19(1):69-72
[4]李明诚.石油与天然气运移(第三版)[M].北京:石油工业出版社,2004
[5]郝石生,黄志龙,杨家琦.天然气运聚动平衡及其应用[M].北京:石油工业出版社,1994
[6]戴金星,宋岩,张厚福.中国大中型气田形成的主要控制因素[J].中国科学(D辑),1996,26(6):481-487
[7]宋岩,戴金星,李先奇,等.中国大中型气田主要地球化学和地质特征[J].石油学报,1998,19(1):1-5
[8]杨俊杰,谢庆邦,宋国初.鄂尔多斯盆地奥陶系风化壳古地貌成藏模式及气藏序列[J].天然气工业,1992,12(4):8-13
[9]宋岩,戴金星,戴春森,等.我国大中型气田主要成藏模式及其分布规律[J].中国科学(D辑),1996,26(6):499-503
[10]何家雄,陈红莲,陈刚,等.莺歌海盆地泥底辟带天然气成藏条件及勘探方向[J].中国海上油气(地质),1995,9(3):157-163
[11]胡光灿,谢姚祥.中国四川盆地东部高陡构造石炭系气田[M].北京:石油工业出版社,1997
[12]蒋有录,张一伟,冉隆辉,等.川东地区志留系-石炭系含气系统天然气运移聚集机理[J].2001,22(1):25-30
[13]郝石生,陈章明,高耀斌,等.天然气藏的形成与保存[M].北京:石油工业出版社,1995
[14] A.佩罗东著.石油地质动力学[M].冯增模译.北京:石油工业出版社,1993.51-57
[15]戴金星,王庭斌,等.中国大中型气田形成条件与分布规律[M].北京:地质出版社, 1997.20-27
[16]戴金星,卫延召,赵靖舟.晚期成藏对大气田形成的重大作用[J].中国地质,2003,30(1):10-18
[17]赵文智,窦立荣,宋岩.我国天然气地质研究与勘探的新进展[J].天然气工业,2000,20(3):1-6
[18] Klemme H D, Ulmishek G F.Effective petroleum source rocks of the world:Stratigraphic distribution and controlling depositional factors[J].AAPG Bulletin, 1991:1809-1851
[19]王涛.中国深盆气田[M].北京:石油工业出版社,2002
[20]宋岩,洪峰.四川盆地川西坳陷深盆气地质条件分析[J].石油勘探与开发,2001,28(2):11-14
[21]张金川,金之均,庞雄奇.深盆气成藏条件及其内部特征[J].石油实验地质,2000,22(3):210-214.
[22]金之钧,张金川,王志欣.深盆气成藏关键地质问题[J].地质论评,2003,49(4):400-406
[23]贾承造,赵文智,魏国齐,等.国外天然气勘探与研究最新进展及发展趋势[J].天然气工业,2002,22(4):5-9
[24]牛嘉玉,王玉满,谯汉生.中国东部老油区深层油气勘探潜力分析[J].中国石油勘探,2004,9(1):33-40
[25]李春光.论渤海湾盆地深层油气勘探[J].海相油气地质,2005,10(2):17-21
[26]何海清,王兆云,程玉群.渤海湾盆地深层石油地质条件分析[J].沉积学报,1999,17(2):273-279
[27]何海清,王兆云,韩品龙.渤海湾盆地深层油气藏类型及油气分布规律[J].石油勘探与开发,1998,25(3):6-9
[28]康竹林.渤海湾盆地深层油气勘探前景.石油勘探与开发[J].2003,23(6):20-22
[29]妥进才,王先彬,周世新.渤海湾盆地深层油气资源前景分析[J].天然气地球科学,1999,10(6):27-31
[30]王玉满,牛嘉玉,谯汉生.渤海湾盆地深层油气资源潜力分析与认识[J].石油勘探与开发,2002,29(2):21-24
[31]樊庆真,杨显成.济阳坳陷深层资源潜力和有利勘探方向[J].石油勘探与开发,1998,25(1):8-10
[32]宋明水,张学才.济阳坳陷渤南洼陷深层天然气的地球化学特征及成因探讨[J].天然气地球科学,2004,15(6):646-649
[33]康竹林.中国深层天然气勘探前景[J].天然气工业,2000,20(5):1-4
[34]谯汉生,方朝亮,牛嘉玉,等.渤海湾盆地深层石油地质[M].北京:石油工业出版社,2002
[35]石昕,戴金星,赵文智.深层油气藏勘探前景分析[J].中国石油勘探,2005,(1):1-10
[36] McTavish R A.Pressure retardation of vitrinite diagenesis, off-shore northwest Europe[J].Nature,1978,271:648-650
[37] Price L C, Wenger L M. The influence of pressure on petroleum generation and maturation as suggested by aqueous pyrolysis [J].Org Geochem,1992,19: 141-159.
[38] Hao F,Sun Y C,Li S T,et al.Overpressure retardation of organic-matter maturation and hydrocarbon generation:a case study from the Yinggehai and Qiongdongnan basins,offshore South China Sea [J].AAPG Bulletin,1995,79:551-562
[39]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
[40]李小地.中国深部油气藏的形成与分布初探[J].石油勘探与开发,1994,21(1):34-39
[41]Р.Т.Самвелов著,王金槊译.深部油气藏的形成分布特征[J].石油地质信息,1996,17(3):133-139
[42]姚超,杜小弟.深层油气勘探[M].北京:石油工业出版社,2002.12
[43]谯汉生,李峰.深层石油地质与勘探[J].勘探家,2000,5(4):10-15
[44]陈中红,查明.东营凹陷流体超压封存箱与油气运聚[J].沉积学报,2006,24(4):607-615
[45]鲍晓欢,郝芳,方勇,等.东营凹陷超压系统的幕式排烃[J].地球科学—中国地质大学学报,2007,32(2):241-246
[46]王涛.中国天然气地质理论基础与实践[M].北京:石油工业出版社,1997
[47]戴金星,戚厚发,王少昌,等.我国煤系的气油地球化学特征、煤成气藏形成条件及资源评价[M].北京:石油工业出版社,2001
[48]朱家蔚,徐永昌,申建中,等.东濮凹陷天然气氩同位素特征及煤成气判识[J].科学通报,1984,(1):41-44
[49]彭君,武晓玲.东濮凹陷马厂地区油气聚集规律[J].山东科技大学学报(自然科学版),2003,22(1):100-103
[50]赵林,夏新宇,戴金星,等.鄂尔多斯盆地上古生界天然气富集的主要控制因素[J].石油实验地质,2000,22(2):136-166
[51] Hunt J M.Petroleum geochemistry and geology[M].W H Freeman and Company,San Francisco,1979
[52] Connan J,Le Tran K and Van Der Weide B.Alteration of petroleum in reservoirs.In: 9th World Petroleum Congress,Proc.,Vol.2,171-178.Lodon:Applied Science Publishers,1975
[53]戴金星,裴锡古,戚厚发.中国天然气地质学(卷一)[M].北京:石油工业出版,1992
[54]徐永昌.天然气成因理论及应用[M].北京:科学出版社,1994
[55]赵孟军,张水昌,廖志勤.原油裂解气在天然气勘探中的意义[J].石油勘探与开发,2001,28(4):47-49
[56] Behar F, Kressmann S, Rudkiewicz J L and Vandenbroucke M.Experimental simulation in confined system and kinetic modeling of kerogen and oil cracking[J].Organic Geochemistry,1991,19:173-189.
[57]胡国艺,肖中尧,罗霞,等.两种裂解气中轻烃组成差异性及其应用[J].天然气工业,2005,25(9):23-25
[58]赵孟军,曾凡刚,秦胜飞,等.塔里木发现和证实两种裂解气[J].天然气工业,2001, 21(1): 35-39·
[59]周兴熙.塔里木盆地台盆区裂解气富集条件[J].天然气工业.1999,19(2): 24-28
[60]谢增业,田世澄,魏国齐,等.川东北飞仙关组储层沥青与古油藏研究[J].天然气地球科学,2005,16(3):283-288
[61]周兴熙.库车油气系统烃类的流体相态特征研究[J].天然气工业,2001,21(2): 82-85
[62]周兴熙.库车油气系统油气藏相态分布及其控制因素[J].天然气地球科学,2004,15 (3):205-213
[63]戴金星.国外的煤成气和主要的聚煤盆地.天然气地质和地球化学论文集(卷三)北京:石油工业出版社,2002
[64]哈尔布特.M.T.等.大油田地质学[M].兰州:甘肃人民出版社1979,1-30,93-106
[65]张子枢,编.世界大气田概论[M].北京:石油工业出版社,1990.8
[66]蒋有录.渤海湾盆地天然气聚集带特征及形成条件[J].石油大学学报(自然科学版),1999,23(5):9-13
[67]梁生正,谢恭俭,马郡,等.华北石炭-二叠系残留盆地天然气勘探方向[J].天然气工业,1998,18(6):16-20
[68]梁宏斌,降栓奇,杨桂茹,等.冀中坳陷北部天然气类型、成藏模式及成藏条件研究[J].中国石油勘探,2002,7(1):17-33
[69]苏立萍,罗平,邹伟宏,等.冀中坳陷斜坡带奥陶系潜山油气成藏条件分析[J].大地构造与成矿学,2003,27(2):191-196
[70]蒋有录.东濮凹陷煤成气、凝析气成藏机理研究[R].山东:中国石油大学(华东),2006
[71]胡文海,陈冬晴,主编.美国油气田分布规律和勘探经验[M].北京:石油工业出版社,1995.5
[72]邵奎政,梁晓东.徐家围子地区天然气成藏期次及其模式[J].大庆石油地质与开发,2002,21(6):4-5
[73]王树学,周庆华,周庆强,等.松辽盆地徐家围子断陷深层天然气含气系统与成藏机制[J].天然气地球科学,2007,18(3):394-398
[74]彭传圣.济阳坳陷孤北低潜山煤成气成藏条件及特征[J].中国海洋大学学报,2005,35(4):670-675
[75]李增学,曹忠祥,余继峰,等.济阳坳陷煤成气富集成藏的盆地动力学特征[J].煤田地质与勘探,2006,34(4):26-29
[76]李红梅.孤北斜坡带煤成气成藏条件分析[J].天然气工业,2006,26(2):23-25
[77]李丕龙,张善文,王永诗,等.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
[78]吴智平,李伟,郑德顺,等.沾化凹陷中、新生代断裂发育及其形成机制分析[J].高校地质学报,2004,10(3):405-417
[79]吴智平,李伟,任拥军,等.济阳坳陷中生代盆地演化及其与新生代盆地的叠合关系探讨[J].地质学报,2003,77(2):281-286
[80]林会喜,方旭庆,李凌,等.鲁北济阳坳陷沾化凹陷东部潜山的发育及油气成藏控制因素.地质通报,2006,25(9-10):1160-1167
[81]王力,金强,林腊梅,等.济阳坳陷孤北—渤南地区渤古4潜山天然气地球化学特征及气源探讨[J].天然气地球科学,2007,18(5):715-749
[82]宫秀梅,金之钧,曾溅辉,等.渤南洼陷深层油气成藏特征及主控因素[J].石油与天然气地质,2005,26(4):473-479
[83]王秉海,钱凯.胜利油区地质研究与勘探实践[M].山东东营:石油大学出版社, 1992
[84]王鸿祯,刘本培,主编.地史学教程[M].北京:地质出版社,1980
[85]吴智平,韩文功.济阳坳陷早晚第三纪沉积间断地层剥蚀量研究[J].中国海上油气(地质),2000,14(5):320-323
[86]万从礼.沾化凹陷孤北地区深层气成藏模式研究[R].山东:胜利油田博士后工作站,2007
[87]金强,等.胜利山东探区中深层天然气成因的地质地球化学研究[R].山东:中国石油大学(华东),2006
[88]林武,李政,李钜源,等.济阳坳陷孤北潜山带天然气成因类型及分布规律[J].石油与天然气地质,2007,28(3):419-426
[89] Thompson,K.F.M,1979,light hydrocarbon in subsurface sediments[J], Geochim. Cosmochim.Acta,43:647-627
[90]张照录,王华,杨红.含油气盆地的输导体系研究.石油与天然气地质,2000,21(2):133-135
[91]付广,薛永超,付晓飞.油气运移输导系统及其对成藏的控制[J].新疆石油地质,2001,22(1):24-26
[92] L.B.马贡,W.G道主编.张刚译.含油气系统—从烃源岩到圈闭[M].北京:石油工业出版社,1998:3-25
[93]卓勤功,宁方兴,容娜.断陷盆地输导体系类型及控藏机制[J].地质评论,2005,51(4):416-422
[94]熊伟.断陷盆地输导体系宏观格架及构成特征—以东营凹陷为例[J].石油勘探与开发.2006,33(4):474-478
[95]王永诗,郝雪峰.济阳断陷湖盆输导体系研究与实践[J].成都理工大学学报(自然科学版).2007,34(4):394-400
[96]罗文生,张善文,王永诗,等.渤南洼陷古近系—新近系断层活动与油气成藏油气[J] .地质与采收率,2007,14(3):34-37
[97]谢启超,刘震,李亮,等.渤南凹陷构造演化与超压形成及演化过程的关系分析[J].西安石油大学学报(自然科学版),2004,19(5):6-10
[98] Losh S,Eglinton L,Schoell M,et al.Vertical and lateral fluid flow related to a large growth fault,South Eugene Island Block 330 Field, Offshore Louisiana[J].AAPG Bulletin,1999,83:244-276
[99]鲁雪松,蒋有录,吴伟.对断层开启机制的再认识[J].油气地质与采收率,2004,11(6):7-9
[100]曾溅辉,邱楠生,宫秀梅,等.济阳、昌潍坳陷深层(Ek-Es4)油气成藏机理及模拟实验研究[R].2003
[101] Powley.D.E. Pressures and hydrogeology in petroleum basins[J].Earth-Science Reviews,1990,29:215-226.
[102]王东晔,查明,吴孔友.有关断层封闭性若干问题的探讨[J].新疆石油地质.2007,28(4):513-520
[103]李丕龙,庞雄奇.陆相断陷盆地隐蔽油气藏形成-以济阳坳陷为例[M].北京:石油工业出版社,2004
[104]宫秀梅,曾溅辉.渤南洼陷古近系膏盐层对深层油气成藏的影响[J],石油勘探与开发,2003,30(5):24-27
[105]ЕременкоНА,ЬотневаТА.深部油气藏[J].ГеологияНефтииГаза,1998,(1):6-11
[106]赵忠新,王华,郭齐军,等.油气输导体系的类型及其输导性能在时空上的演化分析[J].石油实验地质,2002,24(6):527-532.
[107]谢泰俊,潘祖荫,杨学昌.油气运移动力及通道体系[A].南海北部大陆边缘盆地分析与油气聚集[C].北京:科学出版社,1997,385-405.
[108] Galeazzi J S.Structural and stratigraphic evolution of the western Malvinas basin, Argentina[J].AAPG Bulletin,1998,82(4):596-636
[109]林成焰,等.胜利山东探区中深层天然气储层地质研究[R].中国石油大学(华东),2007
[110]向奎,樊庆真,骆光华.应用多元信息综合分析法进行气源追踪—以济阳坳陷深层气气源追踪为例[J].石油实验地质,1998,20(3):261-266
[111]黄志龙,柳广弟,郝石生.东方1-1气田天然气运移地球化学特征[J].沉积学报,1997,15(2): 66-69
[112]郝石生,陈章明,高耀斌,等.天然气藏的形成和保存[M].北京:石油工业出版社,1995.28-35
[113]陈安定.陕甘宁盆地中部气田奥陶系天然气的成因及运移[J],石油学报,1994,15(2):1-10.
[114]张同伟,陈践发,王先彬等.天然气运移的气体同位素地球化学示踪[J].沉积学报,1995,13(2):70-76
[115] Stahl W J . Carbon and Nitrogen Isotopes in Hydrocarbon Research and Exploration[J].Chem. Geol.,1979,20(1)
[116] James A T.Correlation of Natural Gas Using the Carbon Isotopic Distribution Between Hydrocarbon Components[J].AAPG Bulletin,1983,67(1)
[117] Schoell M. Genetic Characterization of Natural Gases[J].AAPG Bulletin.,1983,67:2225-2238
[118]戴金星等.天然气碳氢同位素特征和各类天然气鉴别[J].天然气地球科学,1993,(5)
[119]王廷栋,蔡开平.生物标志物在凝析气藏天然气运移和气源对比中的应用[J].石油学报,1990,11(1):25-31
[120]王顺玉,王廷栋,明巧.高演化地区煤系凝析油的地球化学特征[J].天然气工业,1994,14(2):26-29
[121]陈世佳,代鸿鸣,王廷栋.天然气储层沥青的生标物分布与干气运移[J].西南石油学院学报,1993,15(特刊):60-62
[122]胡守志,付晓文,王廷栋.利用储集层沥青特征识别高演化地区的气层[J].新疆石油地质,2006,27(4):429-431
[123]李延钧,杨远聪,王廷栋,等.生物标志化合物在高熟─过熟气源研究中的应用[J].新疆石油地质,1994,15(1):328-334
[124] K.E.彼得斯,J.M.莫尔多万.生物标记化合物指南-古代沉积物和石油中分子化石的解释[M].北京:石油工业出版社,1995;82-145
[125]侯读杰,张林晔编.实用油气地球化学图鉴[M].北京:石油工业出版社,2003.127-133
[126]付广,孙永河,吕延防.输导通道类型对天然气聚集效率的影响[J].地质论评,2006,52(2):236-243
[127]罗群,庞雄奇,姜振学.一种有效追踪油气运移轨迹的新方法—断面优势运移通道的提出及其应用[J].地质论评,2005,51(2):156-162
[128] Hindle . A . D Petroeum migration pathways and charge concentration : a three-dimensional model[J].AAPG Bulletin,1997,81(9):1451-1481
[129]孙永河,吕延防,付广,等.断裂输导体系输导天然气效率评价方法及其应用[J].天然气地球科学,2006,17(1):73-77
[130] Hull J. Thickness-displacement relationship for deformation zone[J].J Struct Geol.1988, 10, 421-430
[131]柳广弟,李剑,李景明,等.天然气成藏过程有效性的主控因素与评价方法[J].天然气地球科学,2005,16(1):1-6
[132] Burnharn A. K. A simple kinetic model of petroleum formation and cracking[J].Geochim. Cosmo. chim Acta, 1989, 43:1979-1988
[133] James A T.Correlation of natural gas by use of carbon isotopic distribution between hydrocarbon components[J].AAPG Bull,1983:67(7):1176-1191
[134] James A T.Correlation of reservoired gases using the carbon isotopic compositions of wet gas components[J].AAPG Bull, 1990;74(9):1441-1458
[135] Prinzhofer A A and Huc A Y.Genetic and postgenetic molecular and isotopic fractions in natural gas[J].Chemical Geology.1995,126(4):281-290
[136]王振平,付晓泰,卢双舫,等.原油裂解成气模拟实验、产物特征及其意义[J].天然气工业,2001,21(3):11-14
[137]张水昌,赵文智,王飞宇,等.塔里木盆地东部地区古生界原油裂解气成藏历史分析:以英南2气藏为例[J].天然气地球科学,2004,15(5):441-450
[138]陈世加,付晓文,马力宁,等.干酪根裂解气和原油裂解气的成因判识方法[J].石油实验地质,2002,24(4):364-366
[139]侯读杰,赵增迎,唐友军,等.柯克亚地区原油裂解气的地质—地球化学特征[J].天然气地球科学, 2004,15(2):137-141
[140]赵文智,王兆云,张水昌,等.油裂解生气是海相气源灶高效成气的重要途径[J].科学通报,2006,51(5):588-595
[141]王红军,周兴熙.塔里木盆地典型海相成因天然气藏成藏模式[J].石油学报,2001,22(1):14-18.
[142] Lorant F, Prinzhofer A, Behar F,et al. Carbon isotope and molecular constraints on the formation and the expulsion of thermogenic hydrocarbon gases[J].Chem Geol, 1998,147:249-264
[143]李剑,等.济阳坳陷不同类型天然气成因机制及气田形成有利条件分析[R].北京:中国地质大学(北京),2005
[144] Eadington P J, et al. Identifying oil well sites[J].United States Patent Application, 1996,5: 543-616
[145] Eisk M,Eadington P J.Oil migration in the Carticr Trough,Vulcan Sub-basin In: Purcell P G and R.R(eds)[J].The sedimentary basins of W A,Pro-Cccdings, PESA Symposium,1994,Perth 301-312
[146]尹丽娟,张金功,吴汉宁,等.孤北古1井上古生界煤成气藏成藏特征分析[J].西北大学学报(自然科学版),2007,37(1):86-90
[147]陈红汉,等.“相—势”成藏中古流体势场的量化研究[R].湖北:中国地质大学(武汉),2007
[2]张义纲著.天然气的生成聚集与保存[M].南京:河海大学出版社,1991,49-157
[3]蒋有录,张一伟.天然气藏与油藏形成机理及分布特征的异同[J].地质科技情报,2000,19(1):69-72
[4]李明诚.石油与天然气运移(第三版)[M].北京:石油工业出版社,2004
[5]郝石生,黄志龙,杨家琦.天然气运聚动平衡及其应用[M].北京:石油工业出版社,1994
[6]戴金星,宋岩,张厚福.中国大中型气田形成的主要控制因素[J].中国科学(D辑),1996,26(6):481-487
[7]宋岩,戴金星,李先奇,等.中国大中型气田主要地球化学和地质特征[J].石油学报,1998,19(1):1-5
[8]杨俊杰,谢庆邦,宋国初.鄂尔多斯盆地奥陶系风化壳古地貌成藏模式及气藏序列[J].天然气工业,1992,12(4):8-13
[9]宋岩,戴金星,戴春森,等.我国大中型气田主要成藏模式及其分布规律[J].中国科学(D辑),1996,26(6):499-503
[10]何家雄,陈红莲,陈刚,等.莺歌海盆地泥底辟带天然气成藏条件及勘探方向[J].中国海上油气(地质),1995,9(3):157-163
[11]胡光灿,谢姚祥.中国四川盆地东部高陡构造石炭系气田[M].北京:石油工业出版社,1997
[12]蒋有录,张一伟,冉隆辉,等.川东地区志留系-石炭系含气系统天然气运移聚集机理[J].2001,22(1):25-30
[13]郝石生,陈章明,高耀斌,等.天然气藏的形成与保存[M].北京:石油工业出版社,1995
[14] A.佩罗东著.石油地质动力学[M].冯增模译.北京:石油工业出版社,1993.51-57
[15]戴金星,王庭斌,等.中国大中型气田形成条件与分布规律[M].北京:地质出版社, 1997.20-27
[16]戴金星,卫延召,赵靖舟.晚期成藏对大气田形成的重大作用[J].中国地质,2003,30(1):10-18
[17]赵文智,窦立荣,宋岩.我国天然气地质研究与勘探的新进展[J].天然气工业,2000,20(3):1-6
[18] Klemme H D, Ulmishek G F.Effective petroleum source rocks of the world:Stratigraphic distribution and controlling depositional factors[J].AAPG Bulletin, 1991:1809-1851
[19]王涛.中国深盆气田[M].北京:石油工业出版社,2002
[20]宋岩,洪峰.四川盆地川西坳陷深盆气地质条件分析[J].石油勘探与开发,2001,28(2):11-14
[21]张金川,金之均,庞雄奇.深盆气成藏条件及其内部特征[J].石油实验地质,2000,22(3):210-214.
[22]金之钧,张金川,王志欣.深盆气成藏关键地质问题[J].地质论评,2003,49(4):400-406
[23]贾承造,赵文智,魏国齐,等.国外天然气勘探与研究最新进展及发展趋势[J].天然气工业,2002,22(4):5-9
[24]牛嘉玉,王玉满,谯汉生.中国东部老油区深层油气勘探潜力分析[J].中国石油勘探,2004,9(1):33-40
[25]李春光.论渤海湾盆地深层油气勘探[J].海相油气地质,2005,10(2):17-21
[26]何海清,王兆云,程玉群.渤海湾盆地深层石油地质条件分析[J].沉积学报,1999,17(2):273-279
[27]何海清,王兆云,韩品龙.渤海湾盆地深层油气藏类型及油气分布规律[J].石油勘探与开发,1998,25(3):6-9
[28]康竹林.渤海湾盆地深层油气勘探前景.石油勘探与开发[J].2003,23(6):20-22
[29]妥进才,王先彬,周世新.渤海湾盆地深层油气资源前景分析[J].天然气地球科学,1999,10(6):27-31
[30]王玉满,牛嘉玉,谯汉生.渤海湾盆地深层油气资源潜力分析与认识[J].石油勘探与开发,2002,29(2):21-24
[31]樊庆真,杨显成.济阳坳陷深层资源潜力和有利勘探方向[J].石油勘探与开发,1998,25(1):8-10
[32]宋明水,张学才.济阳坳陷渤南洼陷深层天然气的地球化学特征及成因探讨[J].天然气地球科学,2004,15(6):646-649
[33]康竹林.中国深层天然气勘探前景[J].天然气工业,2000,20(5):1-4
[34]谯汉生,方朝亮,牛嘉玉,等.渤海湾盆地深层石油地质[M].北京:石油工业出版社,2002
[35]石昕,戴金星,赵文智.深层油气藏勘探前景分析[J].中国石油勘探,2005,(1):1-10
[36] McTavish R A.Pressure retardation of vitrinite diagenesis, off-shore northwest Europe[J].Nature,1978,271:648-650
[37] Price L C, Wenger L M. The influence of pressure on petroleum generation and maturation as suggested by aqueous pyrolysis [J].Org Geochem,1992,19: 141-159.
[38] Hao F,Sun Y C,Li S T,et al.Overpressure retardation of organic-matter maturation and hydrocarbon generation:a case study from the Yinggehai and Qiongdongnan basins,offshore South China Sea [J].AAPG Bulletin,1995,79:551-562
[39]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
[40]李小地.中国深部油气藏的形成与分布初探[J].石油勘探与开发,1994,21(1):34-39
[41]Р.Т.Самвелов著,王金槊译.深部油气藏的形成分布特征[J].石油地质信息,1996,17(3):133-139
[42]姚超,杜小弟.深层油气勘探[M].北京:石油工业出版社,2002.12
[43]谯汉生,李峰.深层石油地质与勘探[J].勘探家,2000,5(4):10-15
[44]陈中红,查明.东营凹陷流体超压封存箱与油气运聚[J].沉积学报,2006,24(4):607-615
[45]鲍晓欢,郝芳,方勇,等.东营凹陷超压系统的幕式排烃[J].地球科学—中国地质大学学报,2007,32(2):241-246
[46]王涛.中国天然气地质理论基础与实践[M].北京:石油工业出版社,1997
[47]戴金星,戚厚发,王少昌,等.我国煤系的气油地球化学特征、煤成气藏形成条件及资源评价[M].北京:石油工业出版社,2001
[48]朱家蔚,徐永昌,申建中,等.东濮凹陷天然气氩同位素特征及煤成气判识[J].科学通报,1984,(1):41-44
[49]彭君,武晓玲.东濮凹陷马厂地区油气聚集规律[J].山东科技大学学报(自然科学版),2003,22(1):100-103
[50]赵林,夏新宇,戴金星,等.鄂尔多斯盆地上古生界天然气富集的主要控制因素[J].石油实验地质,2000,22(2):136-166
[51] Hunt J M.Petroleum geochemistry and geology[M].W H Freeman and Company,San Francisco,1979
[52] Connan J,Le Tran K and Van Der Weide B.Alteration of petroleum in reservoirs.In: 9th World Petroleum Congress,Proc.,Vol.2,171-178.Lodon:Applied Science Publishers,1975
[53]戴金星,裴锡古,戚厚发.中国天然气地质学(卷一)[M].北京:石油工业出版,1992
[54]徐永昌.天然气成因理论及应用[M].北京:科学出版社,1994
[55]赵孟军,张水昌,廖志勤.原油裂解气在天然气勘探中的意义[J].石油勘探与开发,2001,28(4):47-49
[56] Behar F, Kressmann S, Rudkiewicz J L and Vandenbroucke M.Experimental simulation in confined system and kinetic modeling of kerogen and oil cracking[J].Organic Geochemistry,1991,19:173-189.
[57]胡国艺,肖中尧,罗霞,等.两种裂解气中轻烃组成差异性及其应用[J].天然气工业,2005,25(9):23-25
[58]赵孟军,曾凡刚,秦胜飞,等.塔里木发现和证实两种裂解气[J].天然气工业,2001, 21(1): 35-39·
[59]周兴熙.塔里木盆地台盆区裂解气富集条件[J].天然气工业.1999,19(2): 24-28
[60]谢增业,田世澄,魏国齐,等.川东北飞仙关组储层沥青与古油藏研究[J].天然气地球科学,2005,16(3):283-288
[61]周兴熙.库车油气系统烃类的流体相态特征研究[J].天然气工业,2001,21(2): 82-85
[62]周兴熙.库车油气系统油气藏相态分布及其控制因素[J].天然气地球科学,2004,15 (3):205-213
[63]戴金星.国外的煤成气和主要的聚煤盆地.天然气地质和地球化学论文集(卷三)北京:石油工业出版社,2002
[64]哈尔布特.M.T.等.大油田地质学[M].兰州:甘肃人民出版社1979,1-30,93-106
[65]张子枢,编.世界大气田概论[M].北京:石油工业出版社,1990.8
[66]蒋有录.渤海湾盆地天然气聚集带特征及形成条件[J].石油大学学报(自然科学版),1999,23(5):9-13
[67]梁生正,谢恭俭,马郡,等.华北石炭-二叠系残留盆地天然气勘探方向[J].天然气工业,1998,18(6):16-20
[68]梁宏斌,降栓奇,杨桂茹,等.冀中坳陷北部天然气类型、成藏模式及成藏条件研究[J].中国石油勘探,2002,7(1):17-33
[69]苏立萍,罗平,邹伟宏,等.冀中坳陷斜坡带奥陶系潜山油气成藏条件分析[J].大地构造与成矿学,2003,27(2):191-196
[70]蒋有录.东濮凹陷煤成气、凝析气成藏机理研究[R].山东:中国石油大学(华东),2006
[71]胡文海,陈冬晴,主编.美国油气田分布规律和勘探经验[M].北京:石油工业出版社,1995.5
[72]邵奎政,梁晓东.徐家围子地区天然气成藏期次及其模式[J].大庆石油地质与开发,2002,21(6):4-5
[73]王树学,周庆华,周庆强,等.松辽盆地徐家围子断陷深层天然气含气系统与成藏机制[J].天然气地球科学,2007,18(3):394-398
[74]彭传圣.济阳坳陷孤北低潜山煤成气成藏条件及特征[J].中国海洋大学学报,2005,35(4):670-675
[75]李增学,曹忠祥,余继峰,等.济阳坳陷煤成气富集成藏的盆地动力学特征[J].煤田地质与勘探,2006,34(4):26-29
[76]李红梅.孤北斜坡带煤成气成藏条件分析[J].天然气工业,2006,26(2):23-25
[77]李丕龙,张善文,王永诗,等.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
[78]吴智平,李伟,郑德顺,等.沾化凹陷中、新生代断裂发育及其形成机制分析[J].高校地质学报,2004,10(3):405-417
[79]吴智平,李伟,任拥军,等.济阳坳陷中生代盆地演化及其与新生代盆地的叠合关系探讨[J].地质学报,2003,77(2):281-286
[80]林会喜,方旭庆,李凌,等.鲁北济阳坳陷沾化凹陷东部潜山的发育及油气成藏控制因素.地质通报,2006,25(9-10):1160-1167
[81]王力,金强,林腊梅,等.济阳坳陷孤北—渤南地区渤古4潜山天然气地球化学特征及气源探讨[J].天然气地球科学,2007,18(5):715-749
[82]宫秀梅,金之钧,曾溅辉,等.渤南洼陷深层油气成藏特征及主控因素[J].石油与天然气地质,2005,26(4):473-479
[83]王秉海,钱凯.胜利油区地质研究与勘探实践[M].山东东营:石油大学出版社, 1992
[84]王鸿祯,刘本培,主编.地史学教程[M].北京:地质出版社,1980
[85]吴智平,韩文功.济阳坳陷早晚第三纪沉积间断地层剥蚀量研究[J].中国海上油气(地质),2000,14(5):320-323
[86]万从礼.沾化凹陷孤北地区深层气成藏模式研究[R].山东:胜利油田博士后工作站,2007
[87]金强,等.胜利山东探区中深层天然气成因的地质地球化学研究[R].山东:中国石油大学(华东),2006
[88]林武,李政,李钜源,等.济阳坳陷孤北潜山带天然气成因类型及分布规律[J].石油与天然气地质,2007,28(3):419-426
[89] Thompson,K.F.M,1979,light hydrocarbon in subsurface sediments[J], Geochim. Cosmochim.Acta,43:647-627
[90]张照录,王华,杨红.含油气盆地的输导体系研究.石油与天然气地质,2000,21(2):133-135
[91]付广,薛永超,付晓飞.油气运移输导系统及其对成藏的控制[J].新疆石油地质,2001,22(1):24-26
[92] L.B.马贡,W.G道主编.张刚译.含油气系统—从烃源岩到圈闭[M].北京:石油工业出版社,1998:3-25
[93]卓勤功,宁方兴,容娜.断陷盆地输导体系类型及控藏机制[J].地质评论,2005,51(4):416-422
[94]熊伟.断陷盆地输导体系宏观格架及构成特征—以东营凹陷为例[J].石油勘探与开发.2006,33(4):474-478
[95]王永诗,郝雪峰.济阳断陷湖盆输导体系研究与实践[J].成都理工大学学报(自然科学版).2007,34(4):394-400
[96]罗文生,张善文,王永诗,等.渤南洼陷古近系—新近系断层活动与油气成藏油气[J] .地质与采收率,2007,14(3):34-37
[97]谢启超,刘震,李亮,等.渤南凹陷构造演化与超压形成及演化过程的关系分析[J].西安石油大学学报(自然科学版),2004,19(5):6-10
[98] Losh S,Eglinton L,Schoell M,et al.Vertical and lateral fluid flow related to a large growth fault,South Eugene Island Block 330 Field, Offshore Louisiana[J].AAPG Bulletin,1999,83:244-276
[99]鲁雪松,蒋有录,吴伟.对断层开启机制的再认识[J].油气地质与采收率,2004,11(6):7-9
[100]曾溅辉,邱楠生,宫秀梅,等.济阳、昌潍坳陷深层(Ek-Es4)油气成藏机理及模拟实验研究[R].2003
[101] Powley.D.E. Pressures and hydrogeology in petroleum basins[J].Earth-Science Reviews,1990,29:215-226.
[102]王东晔,查明,吴孔友.有关断层封闭性若干问题的探讨[J].新疆石油地质.2007,28(4):513-520
[103]李丕龙,庞雄奇.陆相断陷盆地隐蔽油气藏形成-以济阳坳陷为例[M].北京:石油工业出版社,2004
[104]宫秀梅,曾溅辉.渤南洼陷古近系膏盐层对深层油气成藏的影响[J],石油勘探与开发,2003,30(5):24-27
[105]ЕременкоНА,ЬотневаТА.深部油气藏[J].ГеологияНефтииГаза,1998,(1):6-11
[106]赵忠新,王华,郭齐军,等.油气输导体系的类型及其输导性能在时空上的演化分析[J].石油实验地质,2002,24(6):527-532.
[107]谢泰俊,潘祖荫,杨学昌.油气运移动力及通道体系[A].南海北部大陆边缘盆地分析与油气聚集[C].北京:科学出版社,1997,385-405.
[108] Galeazzi J S.Structural and stratigraphic evolution of the western Malvinas basin, Argentina[J].AAPG Bulletin,1998,82(4):596-636
[109]林成焰,等.胜利山东探区中深层天然气储层地质研究[R].中国石油大学(华东),2007
[110]向奎,樊庆真,骆光华.应用多元信息综合分析法进行气源追踪—以济阳坳陷深层气气源追踪为例[J].石油实验地质,1998,20(3):261-266
[111]黄志龙,柳广弟,郝石生.东方1-1气田天然气运移地球化学特征[J].沉积学报,1997,15(2): 66-69
[112]郝石生,陈章明,高耀斌,等.天然气藏的形成和保存[M].北京:石油工业出版社,1995.28-35
[113]陈安定.陕甘宁盆地中部气田奥陶系天然气的成因及运移[J],石油学报,1994,15(2):1-10.
[114]张同伟,陈践发,王先彬等.天然气运移的气体同位素地球化学示踪[J].沉积学报,1995,13(2):70-76
[115] Stahl W J . Carbon and Nitrogen Isotopes in Hydrocarbon Research and Exploration[J].Chem. Geol.,1979,20(1)
[116] James A T.Correlation of Natural Gas Using the Carbon Isotopic Distribution Between Hydrocarbon Components[J].AAPG Bulletin,1983,67(1)
[117] Schoell M. Genetic Characterization of Natural Gases[J].AAPG Bulletin.,1983,67:2225-2238
[118]戴金星等.天然气碳氢同位素特征和各类天然气鉴别[J].天然气地球科学,1993,(5)
[119]王廷栋,蔡开平.生物标志物在凝析气藏天然气运移和气源对比中的应用[J].石油学报,1990,11(1):25-31
[120]王顺玉,王廷栋,明巧.高演化地区煤系凝析油的地球化学特征[J].天然气工业,1994,14(2):26-29
[121]陈世佳,代鸿鸣,王廷栋.天然气储层沥青的生标物分布与干气运移[J].西南石油学院学报,1993,15(特刊):60-62
[122]胡守志,付晓文,王廷栋.利用储集层沥青特征识别高演化地区的气层[J].新疆石油地质,2006,27(4):429-431
[123]李延钧,杨远聪,王廷栋,等.生物标志化合物在高熟─过熟气源研究中的应用[J].新疆石油地质,1994,15(1):328-334
[124] K.E.彼得斯,J.M.莫尔多万.生物标记化合物指南-古代沉积物和石油中分子化石的解释[M].北京:石油工业出版社,1995;82-145
[125]侯读杰,张林晔编.实用油气地球化学图鉴[M].北京:石油工业出版社,2003.127-133
[126]付广,孙永河,吕延防.输导通道类型对天然气聚集效率的影响[J].地质论评,2006,52(2):236-243
[127]罗群,庞雄奇,姜振学.一种有效追踪油气运移轨迹的新方法—断面优势运移通道的提出及其应用[J].地质论评,2005,51(2):156-162
[128] Hindle . A . D Petroeum migration pathways and charge concentration : a three-dimensional model[J].AAPG Bulletin,1997,81(9):1451-1481
[129]孙永河,吕延防,付广,等.断裂输导体系输导天然气效率评价方法及其应用[J].天然气地球科学,2006,17(1):73-77
[130] Hull J. Thickness-displacement relationship for deformation zone[J].J Struct Geol.1988, 10, 421-430
[131]柳广弟,李剑,李景明,等.天然气成藏过程有效性的主控因素与评价方法[J].天然气地球科学,2005,16(1):1-6
[132] Burnharn A. K. A simple kinetic model of petroleum formation and cracking[J].Geochim. Cosmo. chim Acta, 1989, 43:1979-1988
[133] James A T.Correlation of natural gas by use of carbon isotopic distribution between hydrocarbon components[J].AAPG Bull,1983:67(7):1176-1191
[134] James A T.Correlation of reservoired gases using the carbon isotopic compositions of wet gas components[J].AAPG Bull, 1990;74(9):1441-1458
[135] Prinzhofer A A and Huc A Y.Genetic and postgenetic molecular and isotopic fractions in natural gas[J].Chemical Geology.1995,126(4):281-290
[136]王振平,付晓泰,卢双舫,等.原油裂解成气模拟实验、产物特征及其意义[J].天然气工业,2001,21(3):11-14
[137]张水昌,赵文智,王飞宇,等.塔里木盆地东部地区古生界原油裂解气成藏历史分析:以英南2气藏为例[J].天然气地球科学,2004,15(5):441-450
[138]陈世加,付晓文,马力宁,等.干酪根裂解气和原油裂解气的成因判识方法[J].石油实验地质,2002,24(4):364-366
[139]侯读杰,赵增迎,唐友军,等.柯克亚地区原油裂解气的地质—地球化学特征[J].天然气地球科学, 2004,15(2):137-141
[140]赵文智,王兆云,张水昌,等.油裂解生气是海相气源灶高效成气的重要途径[J].科学通报,2006,51(5):588-595
[141]王红军,周兴熙.塔里木盆地典型海相成因天然气藏成藏模式[J].石油学报,2001,22(1):14-18.
[142] Lorant F, Prinzhofer A, Behar F,et al. Carbon isotope and molecular constraints on the formation and the expulsion of thermogenic hydrocarbon gases[J].Chem Geol, 1998,147:249-264
[143]李剑,等.济阳坳陷不同类型天然气成因机制及气田形成有利条件分析[R].北京:中国地质大学(北京),2005
[144] Eadington P J, et al. Identifying oil well sites[J].United States Patent Application, 1996,5: 543-616
[145] Eisk M,Eadington P J.Oil migration in the Carticr Trough,Vulcan Sub-basin In: Purcell P G and R.R(eds)[J].The sedimentary basins of W A,Pro-Cccdings, PESA Symposium,1994,Perth 301-312
[146]尹丽娟,张金功,吴汉宁,等.孤北古1井上古生界煤成气藏成藏特征分析[J].西北大学学报(自然科学版),2007,37(1):86-90
[147]陈红汉,等.“相—势”成藏中古流体势场的量化研究[R].湖北:中国地质大学(武汉),2007
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |