临清坳陷上古生界油气资源评价
|
摘要
临清坳陷位于渤海湾裂谷盆地西南收敛端,在中生代以前属于华北地台的一部分。临清地区具有丰富的煤炭资源,在石炭-二叠系发育的煤系烃源岩有机质丰度高、埋藏深、分布广,一直被认为是煤成烃勘探的有利地区。高古4井的钻探成功,证实了临清地区具有良好的勘探前景。
临清坳陷上古生界地层保存较好,石炭-二叠系煤系烃源岩有机质丰度高,厚度大,约800-1200m,且埋藏较深,主要分布在洼陷带,保存条件好,为油气形成提供了良好的物质基础。自石炭-二叠系地层沉积后,临清坳陷在发育过程中经历了多期构造运动,不仅使地质构造异常复杂,而且导致该区的煤系烃源岩多期生、排烃和多期运、聚、散。在沉降时,烃源岩的埋深加大,发生烃类的生、排和运聚成藏作用;上升剥蚀时,生、排烃作用停止,已聚集的油气散失,油气藏被破坏。临清坳陷自海西期以来经过了多期构造作用,使早期形成的单一集中的大油气藏被破坏,油气再次运聚成藏,形成多种分散的小型油气藏,导致油气的分布十分复杂。
本论文在研究了临清地区油气资源评价现状的基础上,遵循临清地区的基本石油地质特征,在叠合单元的基础上,划分出4个较好的评价单元,采用热模拟产烃率法、盆地模拟法和面积丰度类比法三种方法的综合进行油气资源评价,认真客观地选择评价参数进行资源量估算,确定出临清坳陷的资源量为2.782574×108t,最后通过区带评价,提出了高唐-堂邑潜山带、沙镇构造带、德州东部区带、梁村潜山带、铁刘庄构造为首选的有利勘探区块。
Linqing Depression, which belonged to the part of North China Platform in the Mesozoic before, is located in southwest convergence side of the Bohai Bay rift valley basin. Linqing region with abundant coal resources, whose coal hydrocarbon source rocks in Carboniferous–Permian have high abundance of organic matter, buried deep, wide distribution and so on, has been regarded as the most favorable areas in coal-derived hydrocarbon exploration. Drilling success the gaogu 4 well, which confirmed that linqing region has good exploration prospects.
Upper Paleozoic of the Linqing Depression preserved well, Carboniferous-Permian source rocks, with high abundance of organic matter, large thickness, about 800-1200m, and buried deep, which mainly distributed in sub-sag belt, and preservation condition is good, so we can say that Carboniferous-Permian source rocks provides good material base for oil and gas formation. Since the Carboniferous-Permian strata deposited, Linqing depression has experienced multi-stage structural movements during the development, which results in extremely complex geological structure, and leads to source rocks undergo multi-stage generation and expulsion hydrocarbon, and multi-stage migration, gathered and loss. In the settlement, source rocks with the increased depth, commenced the role of generation, expulsion and migration and accumulation; in the erosion, generation and expulsion hydrocarbon stoped, the gathered oil and gas lost, oil and gas reservoirs had been destroyed. Linqing depression has gone though torsional pressure, tension, folding deformation, erosion, and so on, which caused breaking of the early formation of a single centralized large oil and gas reservoirs, so oil and gas went through migration and accumulation again, formed a variety of small reservoirs, which led to the very complex of distribution of oil and gas.
This thesis, based on the studing the status of Linqing region oil and gas resources evaluation, according to the special geologic characteristics of the Linqing area, choose integrated resource evaluation, which synthesizes hydrocarbon production rate of thermal simulation method, basin simulation and analogy method, and chooses carefully and objectively evaluation parameters, estimates resources. Finally, the thesis ascertains that the resources of Linqing depression are about 2.782574×108t, then, carrys out the evaluation zone, proposes the favorable exploration blocks: Gaotang-Tangyi hill zone, Shazhen belt, Dezhou eastern zone, Liangcun hill zone, Tieliuzhuang belt.
临清坳陷上古生界地层保存较好,石炭-二叠系煤系烃源岩有机质丰度高,厚度大,约800-1200m,且埋藏较深,主要分布在洼陷带,保存条件好,为油气形成提供了良好的物质基础。自石炭-二叠系地层沉积后,临清坳陷在发育过程中经历了多期构造运动,不仅使地质构造异常复杂,而且导致该区的煤系烃源岩多期生、排烃和多期运、聚、散。在沉降时,烃源岩的埋深加大,发生烃类的生、排和运聚成藏作用;上升剥蚀时,生、排烃作用停止,已聚集的油气散失,油气藏被破坏。临清坳陷自海西期以来经过了多期构造作用,使早期形成的单一集中的大油气藏被破坏,油气再次运聚成藏,形成多种分散的小型油气藏,导致油气的分布十分复杂。
本论文在研究了临清地区油气资源评价现状的基础上,遵循临清地区的基本石油地质特征,在叠合单元的基础上,划分出4个较好的评价单元,采用热模拟产烃率法、盆地模拟法和面积丰度类比法三种方法的综合进行油气资源评价,认真客观地选择评价参数进行资源量估算,确定出临清坳陷的资源量为2.782574×108t,最后通过区带评价,提出了高唐-堂邑潜山带、沙镇构造带、德州东部区带、梁村潜山带、铁刘庄构造为首选的有利勘探区块。
Linqing Depression, which belonged to the part of North China Platform in the Mesozoic before, is located in southwest convergence side of the Bohai Bay rift valley basin. Linqing region with abundant coal resources, whose coal hydrocarbon source rocks in Carboniferous–Permian have high abundance of organic matter, buried deep, wide distribution and so on, has been regarded as the most favorable areas in coal-derived hydrocarbon exploration. Drilling success the gaogu 4 well, which confirmed that linqing region has good exploration prospects.
Upper Paleozoic of the Linqing Depression preserved well, Carboniferous-Permian source rocks, with high abundance of organic matter, large thickness, about 800-1200m, and buried deep, which mainly distributed in sub-sag belt, and preservation condition is good, so we can say that Carboniferous-Permian source rocks provides good material base for oil and gas formation. Since the Carboniferous-Permian strata deposited, Linqing depression has experienced multi-stage structural movements during the development, which results in extremely complex geological structure, and leads to source rocks undergo multi-stage generation and expulsion hydrocarbon, and multi-stage migration, gathered and loss. In the settlement, source rocks with the increased depth, commenced the role of generation, expulsion and migration and accumulation; in the erosion, generation and expulsion hydrocarbon stoped, the gathered oil and gas lost, oil and gas reservoirs had been destroyed. Linqing depression has gone though torsional pressure, tension, folding deformation, erosion, and so on, which caused breaking of the early formation of a single centralized large oil and gas reservoirs, so oil and gas went through migration and accumulation again, formed a variety of small reservoirs, which led to the very complex of distribution of oil and gas.
This thesis, based on the studing the status of Linqing region oil and gas resources evaluation, according to the special geologic characteristics of the Linqing area, choose integrated resource evaluation, which synthesizes hydrocarbon production rate of thermal simulation method, basin simulation and analogy method, and chooses carefully and objectively evaluation parameters, estimates resources. Finally, the thesis ascertains that the resources of Linqing depression are about 2.782574×108t, then, carrys out the evaluation zone, proposes the favorable exploration blocks: Gaotang-Tangyi hill zone, Shazhen belt, Dezhou eastern zone, Liangcun hill zone, Tieliuzhuang belt.
引文
[1]陈丽.临清坳陷东部断裂活动对中生代盆地的控制作用[J].胜利油田职工大学学报,2008,22(3):131-133.
[2]李孝军.渤海湾盆地临清坳陷东部未熟—低熟油成因探讨[J].天然气地球科学,2009,20(2):273-277.
[3]曹忠祥.临清坳陷东部地区第三系油气勘探问题探讨[J].油气地质与采收率,2003,10(3):17-19.
[4]陈清华,王绍兰,吴孔友.临清坳陷莘县凹陷油气勘探远景评价[J].石油大学学报(自然科学版),1998,22(2):8-10.
[5]杨克绳.再谈临清坳陷古生界油气勘探前景[J].石油地球物理勘探,2006,41(4):476-483.
[6]钱凯,吴世祥,姜正龙,等.华北煤成气成藏条件与勘探目标预测[J].天然气地球科学,1999,10(3-4):35-42.
[7]金强,宋国奇,王力.胜利油田石炭-二叠系煤成气生成模式[J].石油勘探与开发,2009,36(3):358-363.
[8]张鹏飞,陈世悦,张关龙.临清探区石炭-二叠系沉积演化特征[J].中国矿业大学学报,2008,37(2):270-275.
[9]于岚.临清坳陷东部石炭-二叠系煤系烃源岩特征及生烃史[J].新疆石油天然气,2006,2(3):16-22.
[10]刘长江,桑树勋,陈世悦,等.渤海湾盆地石炭-二叠纪成绩作用与储层形成[J].天然气工业,2008,28(4):22-25.
[11]张存霞,吴智平.临清东部中生界垂向地层格架及展布特征[J].断块油气田,2008,15(4):12-15.
[12]张亮,金强.临清坳陷东部太原组煤系烃源岩沉积有机相分析[J].特种油气藏,2009,16(2):23-26.
[13]夏新宇,洪峰,赵林.鄂尔多斯盆地下奥陶统碳酸盐岩有机相类型及生烃潜力[J].沉积学报,1999,17(4):102-106.
[14]彭立才,杨慧珠,刘兰桂,等.柴达木盆地北缘侏罗系烃源岩沉积有机相划分及评价[J].石油与天然气地质,2001,22(2):178-181.
[15]朱德元,牟泽辉.华北地台区石炭-二叠系沉积相[J].石油与天然气地质,1987,8(3):296-305.
[16]李伟,李文涛,柳军.临清坳陷东部断层发育及其对沉积的控制作用[J].西南石油大学学报(自然科学版),2009,31(3):39-44.
[17]吴智平,候旭波,李伟.华北东部地区中生代盆地格局及演化过程探讨[J].大地构造与成矿学,2007,31(4):385-399.
[18]郭绪杰,焦贵浩,姜正龙,等.华北古生界石油地质[M].北京:地质出版社,2002:170-174.
[19]朱炎铭,秦勇,范炳恒,等.渤海湾盆地三叠系沉积厚度恢复及其意义[J].中国矿业大学学报,2001,30(2):195-200.
[20]徐春华.临清坳陷(东部)石炭-二叠系煤系烃源岩形成环境及地化特征[J].复式油气田,1995,6(3):30-33.
[21]王力.济阳和临清坳陷深层天然气成因鉴别与生成模式研究[D].中国石油大学(华东)博士学论文,2008.
[22]黄永玲,徐春华.临清坳陷东部石炭-二叠系煤层综合识别技术[J].石油勘探与开发,1995,22(4):20-23.
[23]张善文,隋风贵.渤海湾盆地前古近系油气地质与远景评价[R].北京:地质出版社,2009:355-357.
[24]徐春华,宋国奇,项希勇.临清坳陷东部古生代煤成气成藏条件[J].海洋石油,2002,(1):6-12.
[25]王兆云,何海清,程克明.华北区古生界原生油气藏勘探前景[J].石油学报,1999,20(2):1-6.
[26]中原油田分公司勘探开发科学研究院.临清坳陷古生界煤成气勘探潜力分析[R].内部报告,2004.
[27]张英利,赵长毅,朱炎铭.华北地区上古生界二次生烃及成藏条件特征[J].沉积学报,2006,24(10):748-752.
[28]张万选.“油气资源评价”的发展与展望[J].断块油气田,1991,1(1):38-40.
[29]郭建宇,张大林,邓宏文,等.低勘探程度区域资源评价方法[J].油气地质与采收率,2006,13(6):43-45.
[30] White David, Harry M.Gehman.Methods of estimating oil and gas resources [J]. AAPGBulletin, 1979, 63(12):2183-2192.
[31] Robert A. Meneley, Alfred E. Calverley, Kenneth G.Logan and Ricard M.Procter. Assessment Methodologies: Current status and future direction [J]. AAPG, 2003, 87 (4):535-540.
[32]肖国林,周才凡.油气资源补充评价方法探讨[J].青岛海洋大学学报,2002,32(3):434-440.
[33]金之钧,张金川.油气资源评价方法的基本原则[J].石油学报,2002,23(1):19-23.
[34]徐春华,徐佑德,邱连贵,等.油气资源评价的现状与发展趋势[J].海洋石油,2001,(4):1-5.
[35] Robert Crovelli, Richard Balay. FASP, an analytic resource appraisal program for petroleum play analysis. Computers&Geoscience, 1986, 12(48):423-475.
[36]张波,刘长,姚剑.盆地模拟技术在禹城地区的应用[J].重庆科技学院学报(自然科学版),2005,7(2):32-33.
[37]石广仁.油气盆地模拟数值方法(第二版)[M].北京:石油工业出版社,1999.
[38]庞雄奇,陈章明,陈发景.含油气盆地地史、热史、生排烃史数值研究与烃源岩评价[C].北京:地质出版社,1993.
[39]庞雄奇,金之钧,姜振学,等.叠合盆地油气资源评价问题及研究意义[J].石油勘探与开发,2002,29(1):9-13.
[40]高岗,柳广弟.资源评价中油气生成定量模型的建立[J].天然气工业,2006,26(10):6-8.
[41]祝厚勤,庞雄奇,姜振学,等.油气聚集系数的研究方法及应用[J].地球科学—中国地质大学学报,2007,32(2):260-265.
[42]柳广弟,赵文智,胡素云,等.油气运聚单元石油运聚系数的预测模式[J].石油勘探与开发,2003,30(5):53-55.
[43]乔永富,毛小平,辛广柱.油气运移聚集定量化模拟[J].地球科学—中国地质大学学报,2005,30(5):617-622.
[44]钱伟,陆现彩.蒙特卡罗法油气资源评价软件的设计与开发[J].江苏地质,2002,26(3):145-149.
[45] Ronald R. Charpentier, Timothy R. Klett. Monte Carlo simulation method. USGS word petroleum assessment 2000—description and results CD.
[46]姜振学,庞雄奇,金之钧,等.门限控烃作用及有效烃源岩判别研究中的应用[J].地球科学—中国地质大学学报,2002,27(6):689-695.
[47]庞雄奇,陈章明,陈发景.排油气门限的基本概念、研究意义与应用[J].现代地质,1997,11(4):510-521.
[48]庞雄奇.排烃门限控油气理论与应用[M].北京:石油工业出版社,1995:8-88.
[49]付秀丽,庞雄奇,张顺.烃源岩排烃方法研究新进展[J].断块油气田,2006,13(6):7-9.
[50]周杰,庞雄奇.一种生、排烃计算方法探讨与应用[J].石油勘探与开发,2002,29(1):24-27.
[51] EDWORD D PITTMAN. Relationship of porosity and permerability to various parameters derived from mercury injection-capillary pressure curves for sandstore [J]. AAPG Bulletin, 1992, 76(2):191-198.
[52]刘长江,桑树勋,陈世悦,等.渤海湾盆地石炭-二叠纪沉积作用与储层形成[J].天然气工业,2008,28(4):22-25.
[53]周章保.渤海湾盆地临清坳陷构造-热演化与上古生界煤成气成藏[D].中国地质大学博士学位论文,2003.
[54]吕希学.渤海湾盆地临清坳陷东部热演化历史和成烃史[J].地质科学,2006,41(4):676-687.
[55]蒋有录,熊继辉.临清坳陷东部地温及有机质热演化特征[J].石油大学学报(自然科学版),1997,21(1):6-10.
[56]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[J].北京:石油工业出版社,2001:1-62.
[57] Stahl W J, Carey J r B D.Source rock identification by isotope analyses of natural gases from fields in the Vol Verde and Delaware Basins[J].Chem Geol, 1975, 16 (4):257- 267.
[58]中国石化股份有限公司石油勘探开发研究院(无锡实验地质研究所).中国东部有效烃源岩研究及勘探前景评价[R].中国石化集团公司科技项目成果报告,2003:210-215.
[59]许化政,周新科.文留地区石炭-二叠纪煤系生烃史及生烃潜力[J].石油与天然气地质,2004,25(4):400-407.
[60]周海燕,庞雄奇,姜振学,等.石油和天然气运聚效率的主控因素及定量评价[J].石油勘探与开发,2002,29(1):14-18.
[61]胡素云,田克勤,柳广弟,等.刻度区解剖方法与油气资源评价关键参数研究[J].石油学报,2005,26(增刊):49-54.
[62]徐晓尹.渤海湾盆地石炭二叠系原生油气藏成藏作用[D].中国石油大学(北京)硕士论文,2007.
[63]熊利平,王运所,许化政,等.东濮凹陷文留盐下煤成气聚集系数研究[J].石油实验地质,2003,25(1):64-68.
[64]朱家蔚,戚厚发.文留煤成气藏的发现及其对华北盆地找气的意义[J].石油勘探与开发,1983,10(1):4-12.
[65]许化政.文留盐背斜形成与油气富集[J].石油与天然气地质,1988,9(3):288-296.
[66]中原油田勘探局.东濮凹陷油气生成地球化学研究[M].北京:石油工业出版社,1991.
[67]徐春华,孔凡顺,王欣辉.煤层排烃系数的定量计算方法—以临清坳陷东部康古4井为例[J].石油实验地质,2006,28(6):303-305.
[68]罗衍灵,周瑶琪.临清坳陷上古生界排烃量估算[J].低渗透油气田,2010,15(57-58):47-51.
[69]李伟.渤海湾盆地地区中生代盆地演化与前第三系油气勘探[D].中国石油大学(华东)博士论文,2007.
[70]武守城.油气资源评价导论—从“数字地球”到“数字油藏”[M].北京:石油工业出版社,2005:251-266.
[71]张道勇.柴达木盆地西部地区石油资源评价[D].中国石油勘探开发科学研究院硕士学论文,2002.
[2]李孝军.渤海湾盆地临清坳陷东部未熟—低熟油成因探讨[J].天然气地球科学,2009,20(2):273-277.
[3]曹忠祥.临清坳陷东部地区第三系油气勘探问题探讨[J].油气地质与采收率,2003,10(3):17-19.
[4]陈清华,王绍兰,吴孔友.临清坳陷莘县凹陷油气勘探远景评价[J].石油大学学报(自然科学版),1998,22(2):8-10.
[5]杨克绳.再谈临清坳陷古生界油气勘探前景[J].石油地球物理勘探,2006,41(4):476-483.
[6]钱凯,吴世祥,姜正龙,等.华北煤成气成藏条件与勘探目标预测[J].天然气地球科学,1999,10(3-4):35-42.
[7]金强,宋国奇,王力.胜利油田石炭-二叠系煤成气生成模式[J].石油勘探与开发,2009,36(3):358-363.
[8]张鹏飞,陈世悦,张关龙.临清探区石炭-二叠系沉积演化特征[J].中国矿业大学学报,2008,37(2):270-275.
[9]于岚.临清坳陷东部石炭-二叠系煤系烃源岩特征及生烃史[J].新疆石油天然气,2006,2(3):16-22.
[10]刘长江,桑树勋,陈世悦,等.渤海湾盆地石炭-二叠纪成绩作用与储层形成[J].天然气工业,2008,28(4):22-25.
[11]张存霞,吴智平.临清东部中生界垂向地层格架及展布特征[J].断块油气田,2008,15(4):12-15.
[12]张亮,金强.临清坳陷东部太原组煤系烃源岩沉积有机相分析[J].特种油气藏,2009,16(2):23-26.
[13]夏新宇,洪峰,赵林.鄂尔多斯盆地下奥陶统碳酸盐岩有机相类型及生烃潜力[J].沉积学报,1999,17(4):102-106.
[14]彭立才,杨慧珠,刘兰桂,等.柴达木盆地北缘侏罗系烃源岩沉积有机相划分及评价[J].石油与天然气地质,2001,22(2):178-181.
[15]朱德元,牟泽辉.华北地台区石炭-二叠系沉积相[J].石油与天然气地质,1987,8(3):296-305.
[16]李伟,李文涛,柳军.临清坳陷东部断层发育及其对沉积的控制作用[J].西南石油大学学报(自然科学版),2009,31(3):39-44.
[17]吴智平,候旭波,李伟.华北东部地区中生代盆地格局及演化过程探讨[J].大地构造与成矿学,2007,31(4):385-399.
[18]郭绪杰,焦贵浩,姜正龙,等.华北古生界石油地质[M].北京:地质出版社,2002:170-174.
[19]朱炎铭,秦勇,范炳恒,等.渤海湾盆地三叠系沉积厚度恢复及其意义[J].中国矿业大学学报,2001,30(2):195-200.
[20]徐春华.临清坳陷(东部)石炭-二叠系煤系烃源岩形成环境及地化特征[J].复式油气田,1995,6(3):30-33.
[21]王力.济阳和临清坳陷深层天然气成因鉴别与生成模式研究[D].中国石油大学(华东)博士学论文,2008.
[22]黄永玲,徐春华.临清坳陷东部石炭-二叠系煤层综合识别技术[J].石油勘探与开发,1995,22(4):20-23.
[23]张善文,隋风贵.渤海湾盆地前古近系油气地质与远景评价[R].北京:地质出版社,2009:355-357.
[24]徐春华,宋国奇,项希勇.临清坳陷东部古生代煤成气成藏条件[J].海洋石油,2002,(1):6-12.
[25]王兆云,何海清,程克明.华北区古生界原生油气藏勘探前景[J].石油学报,1999,20(2):1-6.
[26]中原油田分公司勘探开发科学研究院.临清坳陷古生界煤成气勘探潜力分析[R].内部报告,2004.
[27]张英利,赵长毅,朱炎铭.华北地区上古生界二次生烃及成藏条件特征[J].沉积学报,2006,24(10):748-752.
[28]张万选.“油气资源评价”的发展与展望[J].断块油气田,1991,1(1):38-40.
[29]郭建宇,张大林,邓宏文,等.低勘探程度区域资源评价方法[J].油气地质与采收率,2006,13(6):43-45.
[30] White David, Harry M.Gehman.Methods of estimating oil and gas resources [J]. AAPGBulletin, 1979, 63(12):2183-2192.
[31] Robert A. Meneley, Alfred E. Calverley, Kenneth G.Logan and Ricard M.Procter. Assessment Methodologies: Current status and future direction [J]. AAPG, 2003, 87 (4):535-540.
[32]肖国林,周才凡.油气资源补充评价方法探讨[J].青岛海洋大学学报,2002,32(3):434-440.
[33]金之钧,张金川.油气资源评价方法的基本原则[J].石油学报,2002,23(1):19-23.
[34]徐春华,徐佑德,邱连贵,等.油气资源评价的现状与发展趋势[J].海洋石油,2001,(4):1-5.
[35] Robert Crovelli, Richard Balay. FASP, an analytic resource appraisal program for petroleum play analysis. Computers&Geoscience, 1986, 12(48):423-475.
[36]张波,刘长,姚剑.盆地模拟技术在禹城地区的应用[J].重庆科技学院学报(自然科学版),2005,7(2):32-33.
[37]石广仁.油气盆地模拟数值方法(第二版)[M].北京:石油工业出版社,1999.
[38]庞雄奇,陈章明,陈发景.含油气盆地地史、热史、生排烃史数值研究与烃源岩评价[C].北京:地质出版社,1993.
[39]庞雄奇,金之钧,姜振学,等.叠合盆地油气资源评价问题及研究意义[J].石油勘探与开发,2002,29(1):9-13.
[40]高岗,柳广弟.资源评价中油气生成定量模型的建立[J].天然气工业,2006,26(10):6-8.
[41]祝厚勤,庞雄奇,姜振学,等.油气聚集系数的研究方法及应用[J].地球科学—中国地质大学学报,2007,32(2):260-265.
[42]柳广弟,赵文智,胡素云,等.油气运聚单元石油运聚系数的预测模式[J].石油勘探与开发,2003,30(5):53-55.
[43]乔永富,毛小平,辛广柱.油气运移聚集定量化模拟[J].地球科学—中国地质大学学报,2005,30(5):617-622.
[44]钱伟,陆现彩.蒙特卡罗法油气资源评价软件的设计与开发[J].江苏地质,2002,26(3):145-149.
[45] Ronald R. Charpentier, Timothy R. Klett. Monte Carlo simulation method. USGS word petroleum assessment 2000—description and results CD.
[46]姜振学,庞雄奇,金之钧,等.门限控烃作用及有效烃源岩判别研究中的应用[J].地球科学—中国地质大学学报,2002,27(6):689-695.
[47]庞雄奇,陈章明,陈发景.排油气门限的基本概念、研究意义与应用[J].现代地质,1997,11(4):510-521.
[48]庞雄奇.排烃门限控油气理论与应用[M].北京:石油工业出版社,1995:8-88.
[49]付秀丽,庞雄奇,张顺.烃源岩排烃方法研究新进展[J].断块油气田,2006,13(6):7-9.
[50]周杰,庞雄奇.一种生、排烃计算方法探讨与应用[J].石油勘探与开发,2002,29(1):24-27.
[51] EDWORD D PITTMAN. Relationship of porosity and permerability to various parameters derived from mercury injection-capillary pressure curves for sandstore [J]. AAPG Bulletin, 1992, 76(2):191-198.
[52]刘长江,桑树勋,陈世悦,等.渤海湾盆地石炭-二叠纪沉积作用与储层形成[J].天然气工业,2008,28(4):22-25.
[53]周章保.渤海湾盆地临清坳陷构造-热演化与上古生界煤成气成藏[D].中国地质大学博士学位论文,2003.
[54]吕希学.渤海湾盆地临清坳陷东部热演化历史和成烃史[J].地质科学,2006,41(4):676-687.
[55]蒋有录,熊继辉.临清坳陷东部地温及有机质热演化特征[J].石油大学学报(自然科学版),1997,21(1):6-10.
[56]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[J].北京:石油工业出版社,2001:1-62.
[57] Stahl W J, Carey J r B D.Source rock identification by isotope analyses of natural gases from fields in the Vol Verde and Delaware Basins[J].Chem Geol, 1975, 16 (4):257- 267.
[58]中国石化股份有限公司石油勘探开发研究院(无锡实验地质研究所).中国东部有效烃源岩研究及勘探前景评价[R].中国石化集团公司科技项目成果报告,2003:210-215.
[59]许化政,周新科.文留地区石炭-二叠纪煤系生烃史及生烃潜力[J].石油与天然气地质,2004,25(4):400-407.
[60]周海燕,庞雄奇,姜振学,等.石油和天然气运聚效率的主控因素及定量评价[J].石油勘探与开发,2002,29(1):14-18.
[61]胡素云,田克勤,柳广弟,等.刻度区解剖方法与油气资源评价关键参数研究[J].石油学报,2005,26(增刊):49-54.
[62]徐晓尹.渤海湾盆地石炭二叠系原生油气藏成藏作用[D].中国石油大学(北京)硕士论文,2007.
[63]熊利平,王运所,许化政,等.东濮凹陷文留盐下煤成气聚集系数研究[J].石油实验地质,2003,25(1):64-68.
[64]朱家蔚,戚厚发.文留煤成气藏的发现及其对华北盆地找气的意义[J].石油勘探与开发,1983,10(1):4-12.
[65]许化政.文留盐背斜形成与油气富集[J].石油与天然气地质,1988,9(3):288-296.
[66]中原油田勘探局.东濮凹陷油气生成地球化学研究[M].北京:石油工业出版社,1991.
[67]徐春华,孔凡顺,王欣辉.煤层排烃系数的定量计算方法—以临清坳陷东部康古4井为例[J].石油实验地质,2006,28(6):303-305.
[68]罗衍灵,周瑶琪.临清坳陷上古生界排烃量估算[J].低渗透油气田,2010,15(57-58):47-51.
[69]李伟.渤海湾盆地地区中生代盆地演化与前第三系油气勘探[D].中国石油大学(华东)博士论文,2007.
[70]武守城.油气资源评价导论—从“数字地球”到“数字油藏”[M].北京:石油工业出版社,2005:251-266.
[71]张道勇.柴达木盆地西部地区石油资源评价[D].中国石油勘探开发科学研究院硕士学论文,2002.