晚二叠世盐亭—蓬溪拉张槽东段特征及其对四川盆地中部长兴组油气成藏的控制作用
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摘要
长期以来,四川盆地中部上二叠统长兴组油气勘探尽管已取得发现,但并未形成大规模产能。现今对川中地区长兴组礁滩体分布特征、晚二叠世"盐亭—蓬溪"拉张槽东段边界特征以及长兴组成藏耦合关系并不清晰。结合最新地震资料,精细刻画出盐亭—蓬溪拉张槽东段最新边界,总结分析四川盆地中部长兴组礁滩体分布规律与油气地质特征。研究表明:①盐亭—蓬溪拉张槽东段南西侧以发育条带状生屑礁滩复合体为主要特征,定名为磨溪生屑滩高带。北东侧以发育透镜状生物礁为主要特征,定名为广安生物礁高带。②盐亭—蓬溪拉张槽对川中地区长兴组厚度及礁滩体分布具有控制作用。拉张槽边界两侧长兴组厚度具有明显差异,礁滩体主要发育在拉张槽两侧长兴组中上部地层中。③盐亭—蓬溪拉张槽对川中地区上二叠统—下三叠统烃源岩分布具有控制作用,拉张槽内部长兴组厚度减薄,而飞仙关组一段厚度明显增大,具备较优质烃源岩发育条件。④四川盆地中部是以下寒武统为主的多源供烃模式,具有垂侧向复合输导系统,长兴组为次生古油藏—原生气藏/次生气藏模式。综上认为,长兴组油气地质特征相较下古生界更为复杂,四川盆地中部长兴组古油藏规模有限,气源不足是现今未大规模成藏的主要原因。烃源岩/优势气源区—输导系统—优质礁滩体储层耦合是寻找长兴组油气勘探"甜点"区的关键。
For a long time,although the Upper Permian was discovered in the Changxing Formation,no large-scale production capacity has been formed.The reef-shoal distribution characteristic of the Changxing Formation,the border of the Late Permian Yanting-Pengxi intracratonic sag and the hydrocarbon accumulation relationship are still not clear.With the latest seismic data,this paper describes the latest boundary of the eastern section of the Yanting-Pengxi intracratonic sag in detail,and summarizes the distribution of reef-shoal body and the geological characteristic of hydrocarbon for the Changxing Formation in the central Sichuan Basin.The results show that:(1)The southwestern side of the Yanting-Pengxi intracratonic sag is characterized by the development of the strip-like complex reef-shoal,which is named as the High Belt of the Moxi Shoal Platform Margin.The northeast side mainly developed the tundra-like reef as the main feature,it is named as the High Belt of the Guang'an Reef Platform Margin.(2)The Yanting-Pengxi sag has a controlling effect on the thickness of the Changxing Formation and the distribution of reef-shoal in the central Sichuan Basin.There are significant thickness differences of the Changxing Formation on the both sides of the intracratonic sag boundary.The reef-shoal are mainly developed in the middle and upper strata of the Changxing Formation.(3)The Yanting-Pengxi Intracratonic sag has a controlling effect on the source rock distribution of the Upper Permianto the Triassic in the central Sichuan Basin.The thickness of the Changxing Formation in the intracratonic sag reduced,while the thickness of the Feixianguan Formation obviously increased,which have the development conditions of high quality source rocks.(4)With multisource hydrocarbon supply model of the Lower Cambrian black shale leading and the vertical-lateral seal bypassing system,the Changxing Formation in the Sichuan Basin is secondary paleo-oil reservoir-original gas reservoir/secondary gas reservoir models.In summary,the geological characteristics of the Changxing Formation in the central Sichuan Basin is more complex than those in the Lower Paleozoic.The paleo-oil reservoirs of the Changxing Formation are currently not a large scale,so that the lack of gas source is the main reason for the lack of large-scale reservoir accumulation.The coupling relationship of good source rocks/gas source areas-seal bypassing system-reef-shoal reservoirs is the key point for"dessert"zone exploration of the Changxing Formation.
For a long time,although the Upper Permian was discovered in the Changxing Formation,no large-scale production capacity has been formed.The reef-shoal distribution characteristic of the Changxing Formation,the border of the Late Permian Yanting-Pengxi intracratonic sag and the hydrocarbon accumulation relationship are still not clear.With the latest seismic data,this paper describes the latest boundary of the eastern section of the Yanting-Pengxi intracratonic sag in detail,and summarizes the distribution of reef-shoal body and the geological characteristic of hydrocarbon for the Changxing Formation in the central Sichuan Basin.The results show that:(1)The southwestern side of the Yanting-Pengxi intracratonic sag is characterized by the development of the strip-like complex reef-shoal,which is named as the High Belt of the Moxi Shoal Platform Margin.The northeast side mainly developed the tundra-like reef as the main feature,it is named as the High Belt of the Guang'an Reef Platform Margin.(2)The Yanting-Pengxi sag has a controlling effect on the thickness of the Changxing Formation and the distribution of reef-shoal in the central Sichuan Basin.There are significant thickness differences of the Changxing Formation on the both sides of the intracratonic sag boundary.The reef-shoal are mainly developed in the middle and upper strata of the Changxing Formation.(3)The Yanting-Pengxi Intracratonic sag has a controlling effect on the source rock distribution of the Upper Permianto the Triassic in the central Sichuan Basin.The thickness of the Changxing Formation in the intracratonic sag reduced,while the thickness of the Feixianguan Formation obviously increased,which have the development conditions of high quality source rocks.(4)With multisource hydrocarbon supply model of the Lower Cambrian black shale leading and the vertical-lateral seal bypassing system,the Changxing Formation in the Sichuan Basin is secondary paleo-oil reservoir-original gas reservoir/secondary gas reservoir models.In summary,the geological characteristics of the Changxing Formation in the central Sichuan Basin is more complex than those in the Lower Paleozoic.The paleo-oil reservoirs of the Changxing Formation are currently not a large scale,so that the lack of gas source is the main reason for the lack of large-scale reservoir accumulation.The coupling relationship of good source rocks/gas source areas-seal bypassing system-reef-shoal reservoirs is the key point for"dessert"zone exploration of the Changxing Formation.
引文
[1]Luo Zhili.The influence on the formation oil and mineral resources from taphrogenesis movement since the Late Paleozoic in southwest China[J].Acta Geologica Sichuan,1981,2(1):1-22.罗志立.中国西南地区晚古生代以来地裂运动对石油等矿产形成的影响[J].四川地质学报,1981,2(1):1-22.
[2]Liu Shugen,Wang Yigang,Sun Wei,et al.Control of intracratonic sags on the hydrocarbon accumulations in the marine strata across the Sichuan Basin,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2016,43(1):1-23.刘树根,王一刚,孙玮,等.拉张槽对四川盆地海相油气分布的控制作用[J].成都理工大学学报:自然科学版,2016,43(1):1-23.
[3]Liu Shugen,Sun Wei,Luo Zhili,et al.Xingkai taphrogenesis and petroleum exploration from Upper Sinian to Cambrian strata in Sichuan Basin,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2013,40(5):511-520.刘树根,孙玮,罗志立,等.兴凯地裂运动与四川盆地下组合油气勘探[J].成都理工大学学报:自然科学版,2013,40(5):511-520.
[4]Liu Shugen,Liu Shu,Sun Wei,et al,Tectonic and sedimentary features of the northern Mianyang-Changning intracratonic sag,Sichuan,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2018,45(1):1-13.刘树根,刘殊,孙玮,等.绵阳-长宁拉张槽北段构造-沉积特征[J].成都理工大学学报:自然科学版,2018,45(1):1-13.
[5]Wang Yigang,Wen Yingchu,Zhang Fan,et al.Distribution law of the organic reefs in Changxing Formation of Upper Permian in east Sichuan[J].Natrual Gas Industry,1998,18(6):7-8,25-30.王一刚,文应初,张帆,等.川东地区上二叠统长兴组生物礁分布规律[J].天然气工业,1998,18(6):7-8,25-30.
[6]Ma Yongsheng,Mou Chuanlong,Tan Qinyin,et al.A discussion on Kaijiang-Liangping ocean trough[J].Oil&Gas Geology,2006,27(3):326-331.马永生,牟传龙,谭钦银,等.关于开江-梁平海槽的认识[J].石油与天然气地质,2006,27(3):326-331.
[7]Huang Renchun.Formation and evolution of Permian-Triassic Kaijiang-Liangping shelf and development of reef-shoal reservoirs in Sichuan Basin[J].Journal of Chengdu University of Technology:Science&Technology Edition,2014,41(4):452-457.黄仁春.四川盆地二叠纪-三叠纪开江-梁平陆棚形成演化与礁滩发育[J].成都理工大学学报:自然科学版,2014,41(4):452-457.
[8]Zhang Qi,Tu Zhihui,Rao Lei,et al.Control of Later Permian Pengxi-Wusheng depressional platform on bioreef and shoal distribution within platform,central Sichuan Basin[J].Natural Gas Exploration and Development,2010,33(4):1-4.张奇,屠志慧,饶雷,等.四川川中地区晚二叠世蓬溪-武胜台凹对台内生物礁滩分布的控制作用[J].天然气勘探与开发,2010,33(4):1-4.
[9]Li Qiufen.Geological Characteristics of Yanting-Tongnan Trough and Distribution of Reef-bank in Central Sichuan Basin[D].Beijing:China University of Geosciences(Beijing),2013.李秋芬.四川盆地盐亭---潼南海槽地质特征及台缘带礁滩体分布特征研究[D].北京:中国地质大学(北京),2013.
[10]Li Qiufen,Miao Shunde,Wang Tongshan,et al.Sedimentary filling configuration of Yangting-Tongnan through under the background of intracratonic rift in Later Permian,Sichuan Basin[J].Earth Science Frontiers,2015,22(1):67-76.李秋芬,苗顺德,王铜山,等.四川盆地晚二叠世克拉通内裂陷作用背景下的盐亭-潼南海槽沉积充填特征[J].地学前缘,2015,22(1):67-76.
[11]Du Jinhu,Wang Zecheng,Zou Caineng,et al.Discovery of intracratonic rift in the Upper Yangtze and its control effect on the Formation of Anyue giant gas field[J].Acta Petrolei Sinica,2016,37(1):1-16.杜金虎,汪泽成,邹才能,等.上扬子克拉通内裂陷的发现及对安岳特大型气田形成的控制作用[J].石油学报,2016,37(1):1-16.
[12]Xu Chunchun,Shen Ping,Yang Yueming,et al.Accumulation conditions and enrichment patterns of natural gas in the Lower Cambrian Longwangmiao Formation reservoirs of the Leshan-Longnvsi Paleohigh,Sichuan Basin[J].Natural Gas Industry,2014,34(3):1-7.徐春春,沈平,杨跃明,等.乐山-龙女寺古隆起震旦系-下寒武统龙王庙组天然气成藏条件与富集规律[J].天然气工业,2014,34(3):1-7.
[13]Li Zhongquan,Liu Ji,Li Ying,et al.Formation and evolution of Weiyuan-Anyue extension-erosion groove in Sinian System,Sichuan Basin[J].Petroleum Exploration and Development,2015,42(1):26-33.李忠权,刘记,李应,等.四川盆地震旦系威远-安岳拉张侵蚀槽特征及形成演化[J].石油勘探与开发,2015,42(1):26-33.
[14]Yang Yueming,Wen Long,Luo Bing,et al.Hydrocarbon accumulation of Sinian natural gas reservoirs,Leshan-Longnvsi Paleohigh,Sichuan Basin,SW China[J].Petroleum Exploration and Development,2016,43(2):179-188.杨跃明,文龙,罗冰,等.四川盆地乐山-龙女寺古隆起震旦系天然气成藏特征[J].石油勘探与开发,2016,43(2):179-188.
[15]Liu Shugen,Deng Bin,Li Zhiwu,et al.The texture of sedimentary basin-orogenic belt system and its influence on oil/gas distribution:A case study from Sichuan Basin[J].Acta Petrologica Sinica,2011,27(3):621-635.刘树根,邓宾,李智武,等.盆山结构与油气分布---以四川盆地为例[J].岩石学报,2011,27(3):621-635.
[16]Zhong Yong,Li Yalin,Zhang Xiaobin,et al.Feature of extensional structures in Pre-Sinian to Cambrian strata,Sichuan Basin,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2013,40(5):498-510.钟勇,李亚林,张晓斌,等.四川盆地下组合张性构造特征[J].成都理工大学学报:自然科学版,2013,40(5):498-510.
[17]Liu Shugen,Sun Wei,Song Jinmin,et al.Tectonic-controlled distribution of marine petroleum accumulation in the Sichuan Basin,China[J].Earth Science Frontiers,2015,22(3):146-160.刘树根,孙玮,宋金民,等.四川盆地海相油气分布的构造控制理论[J].地学前缘,2015,22(3):146-160.
[18]Wang Yigang,Wen Yingchu,Hong Haitao,et al.Dalong Formation found in Kaijiang-Liangping ocenic trough in the Sichuan Basin[J].Natrual Gas Industry,2006,26(9):32-36.王一刚,文应初,洪海涛,等.四川盆地开江-梁平海槽内发现大隆组[J].天然气工业,2006,26(9):32-36.
[19]Xia Maolong,Wen Long,Wang Yigang,et al.High-quality source rocks in trough facies of Upper Permian Dalong Formation of Sichuan Basin[J].Petroleum Exploration and Development,2010,37(6):654-662.夏茂龙,文龙,王一刚,等.四川盆地上二叠统海槽相大隆组优质烃源岩[J].石油勘探与开发,2010,37(6):654-662.
[20]Allen P A,Allen J R.Basin Analysis Principles and Application to Petroleum,Play Assessment[M].Third Edition.London:Jphn Wiley&Sons,Ltd(UK),2013.
[21]Huang Shipeng,Jiang Qingchun,Wang Zecheng,et al.Differences between the Middle Permian Qixia and Maokou source rocks in the Sichuan Basin[J].Natrual Gas Industry,2016,36(12):26-34.黄士鹏,江青春,汪泽成,等.四川盆地中二叠统栖霞组与茅口组烃源岩的差异性[J].天然气工业,2016,36(12):26-34.
[22]Zhang Jian,Zhou Gang,Zhang Guangrong,et al.Geological characteristics and exploration orientation of Mid-Permian natural gas in the Sichuan Basin[J].Natrual Gas Industry,2018,38(1):10-20.张健,周刚,张光荣,等.四川盆地中二叠统天然气地质特征与勘探方向[J].天然气工业,2018,38(1):10-20.
[23]Wang Zecheng,Jiang Qingchun,Huang Shipeng,et al.Geological conditions for massive accumulation of natural gas in the Mid-Permian Maokou Formation of the Sichuan Basin[J].Natrual Gas Industry,2018,38(1):30-38.汪泽成,江青春,黄士鹏,等.四川盆地中二叠统茅口组天然气大面积成藏的地质条件[J].天然气工业,2018,38(1):30-38.
[24]Liu Guangxiang,Jin Zhijun,Deng Mo,et al.Exploration potential for shale gas in the Upper Permian Longtan Formation in eastern Sichuan Basin[J].Natrual Gas Geoscience,2015,36(3):481-487.刘光祥,金之钧,邓模,等.川东地区上二叠统龙潭组页岩气勘探潜力[J].石油与天然气地质,2015,36(3):481-487.
[25]Huang Wenming,Liu Shugen,Wang Guozhi,et al.Geological conditions and gas reservoir features in Lower Paleozoic in Sichuan Basin[J].Natrual Gas Geoscience,2011,22(3):465-476.黄文明,刘树根,王国芝,等.四川盆地下古生界油气地质条件及气藏特征[J].天然气地球科学,2011,22(3):465-476.
[26]Deng Yan,Hu Guoyi,Zhao Changyi.Geochemical characteristics and origin of natural gas in Changxing-Feixianguan Formations from Longgang Gasfield in the Sichuan Basin,China[J].Natural Gas Geoscience,2018,29(6):892-907.邓焱,胡国艺,赵长毅.四川盆地龙岗气田长兴组-飞仙关组天然气地球化学特征及成因[J].天然气地球科学,2018,29(6):892-907.
[27]Xia Guodong,Ran Bo,Liu Shugen,et al.Characteristics of hydrocarbon source rocks of the Lower Cambrian Maidiping Formation in northern Mianyang-Changning intracratonic sag,Sichuan,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2018,45(1):14-26.夏国栋,冉波,刘树根,等.绵阳-长宁拉张槽北段麦地坪组烃源岩特征---以绵竹清平剖面为例[J].成都理工大学学报:自然科学版,2018,45(1):14-26.
[28]Liu Shugen,Sun Wei,Zhao Yihua,et al.Differential accumulation and distribution of natural gas and their main controlling factors in the Upper Sinian Dengying Formation,Sichuan Basin[J].Natural Gas Industry,2015,35(1):10-23.刘树根,孙玮,赵异华,等.四川盆地震旦系灯影组天然气的差异聚集分布及其主控因素[J].天然气工业,2015,35(1):10-23.
[29]Liang Xiao,Liu Shugen,Xia Ming,et al.Characteristics and geological significance of gas chimney of the Sinian Dengying Formation in the Weiyuan structure,Sichuan Basin[J].Oil&Gas Geology,2016,37(5):702-712.梁霄,刘树根,夏铭,等.四川盆地威远构造震旦系灯影组气烟囱特征及其地质意义[J].石油与天然气地质,2016,37(5):702-712.
[30]Wang Guozhi,Liu Shugen.Paleo-fluid geochemical evaluation of hydrocarbon preservation in marine carbonate rock areas:Taking lower association in central Sichuan Basin as an example[J].Journal of Chengdu University of Technology:Science&Technology Edition,2009,36(6):631-634.王国芝,刘树根.海相碳酸盐岩区油气保存条件的古流体地球化学评价---以四川盆地中部下组合为例[J].成都理工大学学报:自然科学版,2009,36(6):631-644.
[31]Liu Shugen,Sun Wei,Wang Guozhi,et al.Analysis of causes of oil and gas accumulation in superimposed Sichuan Basin of China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2013,40(5):481-497.刘树根,孙玮,王国芝,等.四川叠合盆地油气富集原因剖析[J].成都理工大学学报:自然科学版,2013,40(5):481-497.
[2]Liu Shugen,Wang Yigang,Sun Wei,et al.Control of intracratonic sags on the hydrocarbon accumulations in the marine strata across the Sichuan Basin,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2016,43(1):1-23.刘树根,王一刚,孙玮,等.拉张槽对四川盆地海相油气分布的控制作用[J].成都理工大学学报:自然科学版,2016,43(1):1-23.
[3]Liu Shugen,Sun Wei,Luo Zhili,et al.Xingkai taphrogenesis and petroleum exploration from Upper Sinian to Cambrian strata in Sichuan Basin,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2013,40(5):511-520.刘树根,孙玮,罗志立,等.兴凯地裂运动与四川盆地下组合油气勘探[J].成都理工大学学报:自然科学版,2013,40(5):511-520.
[4]Liu Shugen,Liu Shu,Sun Wei,et al,Tectonic and sedimentary features of the northern Mianyang-Changning intracratonic sag,Sichuan,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2018,45(1):1-13.刘树根,刘殊,孙玮,等.绵阳-长宁拉张槽北段构造-沉积特征[J].成都理工大学学报:自然科学版,2018,45(1):1-13.
[5]Wang Yigang,Wen Yingchu,Zhang Fan,et al.Distribution law of the organic reefs in Changxing Formation of Upper Permian in east Sichuan[J].Natrual Gas Industry,1998,18(6):7-8,25-30.王一刚,文应初,张帆,等.川东地区上二叠统长兴组生物礁分布规律[J].天然气工业,1998,18(6):7-8,25-30.
[6]Ma Yongsheng,Mou Chuanlong,Tan Qinyin,et al.A discussion on Kaijiang-Liangping ocean trough[J].Oil&Gas Geology,2006,27(3):326-331.马永生,牟传龙,谭钦银,等.关于开江-梁平海槽的认识[J].石油与天然气地质,2006,27(3):326-331.
[7]Huang Renchun.Formation and evolution of Permian-Triassic Kaijiang-Liangping shelf and development of reef-shoal reservoirs in Sichuan Basin[J].Journal of Chengdu University of Technology:Science&Technology Edition,2014,41(4):452-457.黄仁春.四川盆地二叠纪-三叠纪开江-梁平陆棚形成演化与礁滩发育[J].成都理工大学学报:自然科学版,2014,41(4):452-457.
[8]Zhang Qi,Tu Zhihui,Rao Lei,et al.Control of Later Permian Pengxi-Wusheng depressional platform on bioreef and shoal distribution within platform,central Sichuan Basin[J].Natural Gas Exploration and Development,2010,33(4):1-4.张奇,屠志慧,饶雷,等.四川川中地区晚二叠世蓬溪-武胜台凹对台内生物礁滩分布的控制作用[J].天然气勘探与开发,2010,33(4):1-4.
[9]Li Qiufen.Geological Characteristics of Yanting-Tongnan Trough and Distribution of Reef-bank in Central Sichuan Basin[D].Beijing:China University of Geosciences(Beijing),2013.李秋芬.四川盆地盐亭---潼南海槽地质特征及台缘带礁滩体分布特征研究[D].北京:中国地质大学(北京),2013.
[10]Li Qiufen,Miao Shunde,Wang Tongshan,et al.Sedimentary filling configuration of Yangting-Tongnan through under the background of intracratonic rift in Later Permian,Sichuan Basin[J].Earth Science Frontiers,2015,22(1):67-76.李秋芬,苗顺德,王铜山,等.四川盆地晚二叠世克拉通内裂陷作用背景下的盐亭-潼南海槽沉积充填特征[J].地学前缘,2015,22(1):67-76.
[11]Du Jinhu,Wang Zecheng,Zou Caineng,et al.Discovery of intracratonic rift in the Upper Yangtze and its control effect on the Formation of Anyue giant gas field[J].Acta Petrolei Sinica,2016,37(1):1-16.杜金虎,汪泽成,邹才能,等.上扬子克拉通内裂陷的发现及对安岳特大型气田形成的控制作用[J].石油学报,2016,37(1):1-16.
[12]Xu Chunchun,Shen Ping,Yang Yueming,et al.Accumulation conditions and enrichment patterns of natural gas in the Lower Cambrian Longwangmiao Formation reservoirs of the Leshan-Longnvsi Paleohigh,Sichuan Basin[J].Natural Gas Industry,2014,34(3):1-7.徐春春,沈平,杨跃明,等.乐山-龙女寺古隆起震旦系-下寒武统龙王庙组天然气成藏条件与富集规律[J].天然气工业,2014,34(3):1-7.
[13]Li Zhongquan,Liu Ji,Li Ying,et al.Formation and evolution of Weiyuan-Anyue extension-erosion groove in Sinian System,Sichuan Basin[J].Petroleum Exploration and Development,2015,42(1):26-33.李忠权,刘记,李应,等.四川盆地震旦系威远-安岳拉张侵蚀槽特征及形成演化[J].石油勘探与开发,2015,42(1):26-33.
[14]Yang Yueming,Wen Long,Luo Bing,et al.Hydrocarbon accumulation of Sinian natural gas reservoirs,Leshan-Longnvsi Paleohigh,Sichuan Basin,SW China[J].Petroleum Exploration and Development,2016,43(2):179-188.杨跃明,文龙,罗冰,等.四川盆地乐山-龙女寺古隆起震旦系天然气成藏特征[J].石油勘探与开发,2016,43(2):179-188.
[15]Liu Shugen,Deng Bin,Li Zhiwu,et al.The texture of sedimentary basin-orogenic belt system and its influence on oil/gas distribution:A case study from Sichuan Basin[J].Acta Petrologica Sinica,2011,27(3):621-635.刘树根,邓宾,李智武,等.盆山结构与油气分布---以四川盆地为例[J].岩石学报,2011,27(3):621-635.
[16]Zhong Yong,Li Yalin,Zhang Xiaobin,et al.Feature of extensional structures in Pre-Sinian to Cambrian strata,Sichuan Basin,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2013,40(5):498-510.钟勇,李亚林,张晓斌,等.四川盆地下组合张性构造特征[J].成都理工大学学报:自然科学版,2013,40(5):498-510.
[17]Liu Shugen,Sun Wei,Song Jinmin,et al.Tectonic-controlled distribution of marine petroleum accumulation in the Sichuan Basin,China[J].Earth Science Frontiers,2015,22(3):146-160.刘树根,孙玮,宋金民,等.四川盆地海相油气分布的构造控制理论[J].地学前缘,2015,22(3):146-160.
[18]Wang Yigang,Wen Yingchu,Hong Haitao,et al.Dalong Formation found in Kaijiang-Liangping ocenic trough in the Sichuan Basin[J].Natrual Gas Industry,2006,26(9):32-36.王一刚,文应初,洪海涛,等.四川盆地开江-梁平海槽内发现大隆组[J].天然气工业,2006,26(9):32-36.
[19]Xia Maolong,Wen Long,Wang Yigang,et al.High-quality source rocks in trough facies of Upper Permian Dalong Formation of Sichuan Basin[J].Petroleum Exploration and Development,2010,37(6):654-662.夏茂龙,文龙,王一刚,等.四川盆地上二叠统海槽相大隆组优质烃源岩[J].石油勘探与开发,2010,37(6):654-662.
[20]Allen P A,Allen J R.Basin Analysis Principles and Application to Petroleum,Play Assessment[M].Third Edition.London:Jphn Wiley&Sons,Ltd(UK),2013.
[21]Huang Shipeng,Jiang Qingchun,Wang Zecheng,et al.Differences between the Middle Permian Qixia and Maokou source rocks in the Sichuan Basin[J].Natrual Gas Industry,2016,36(12):26-34.黄士鹏,江青春,汪泽成,等.四川盆地中二叠统栖霞组与茅口组烃源岩的差异性[J].天然气工业,2016,36(12):26-34.
[22]Zhang Jian,Zhou Gang,Zhang Guangrong,et al.Geological characteristics and exploration orientation of Mid-Permian natural gas in the Sichuan Basin[J].Natrual Gas Industry,2018,38(1):10-20.张健,周刚,张光荣,等.四川盆地中二叠统天然气地质特征与勘探方向[J].天然气工业,2018,38(1):10-20.
[23]Wang Zecheng,Jiang Qingchun,Huang Shipeng,et al.Geological conditions for massive accumulation of natural gas in the Mid-Permian Maokou Formation of the Sichuan Basin[J].Natrual Gas Industry,2018,38(1):30-38.汪泽成,江青春,黄士鹏,等.四川盆地中二叠统茅口组天然气大面积成藏的地质条件[J].天然气工业,2018,38(1):30-38.
[24]Liu Guangxiang,Jin Zhijun,Deng Mo,et al.Exploration potential for shale gas in the Upper Permian Longtan Formation in eastern Sichuan Basin[J].Natrual Gas Geoscience,2015,36(3):481-487.刘光祥,金之钧,邓模,等.川东地区上二叠统龙潭组页岩气勘探潜力[J].石油与天然气地质,2015,36(3):481-487.
[25]Huang Wenming,Liu Shugen,Wang Guozhi,et al.Geological conditions and gas reservoir features in Lower Paleozoic in Sichuan Basin[J].Natrual Gas Geoscience,2011,22(3):465-476.黄文明,刘树根,王国芝,等.四川盆地下古生界油气地质条件及气藏特征[J].天然气地球科学,2011,22(3):465-476.
[26]Deng Yan,Hu Guoyi,Zhao Changyi.Geochemical characteristics and origin of natural gas in Changxing-Feixianguan Formations from Longgang Gasfield in the Sichuan Basin,China[J].Natural Gas Geoscience,2018,29(6):892-907.邓焱,胡国艺,赵长毅.四川盆地龙岗气田长兴组-飞仙关组天然气地球化学特征及成因[J].天然气地球科学,2018,29(6):892-907.
[27]Xia Guodong,Ran Bo,Liu Shugen,et al.Characteristics of hydrocarbon source rocks of the Lower Cambrian Maidiping Formation in northern Mianyang-Changning intracratonic sag,Sichuan,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2018,45(1):14-26.夏国栋,冉波,刘树根,等.绵阳-长宁拉张槽北段麦地坪组烃源岩特征---以绵竹清平剖面为例[J].成都理工大学学报:自然科学版,2018,45(1):14-26.
[28]Liu Shugen,Sun Wei,Zhao Yihua,et al.Differential accumulation and distribution of natural gas and their main controlling factors in the Upper Sinian Dengying Formation,Sichuan Basin[J].Natural Gas Industry,2015,35(1):10-23.刘树根,孙玮,赵异华,等.四川盆地震旦系灯影组天然气的差异聚集分布及其主控因素[J].天然气工业,2015,35(1):10-23.
[29]Liang Xiao,Liu Shugen,Xia Ming,et al.Characteristics and geological significance of gas chimney of the Sinian Dengying Formation in the Weiyuan structure,Sichuan Basin[J].Oil&Gas Geology,2016,37(5):702-712.梁霄,刘树根,夏铭,等.四川盆地威远构造震旦系灯影组气烟囱特征及其地质意义[J].石油与天然气地质,2016,37(5):702-712.
[30]Wang Guozhi,Liu Shugen.Paleo-fluid geochemical evaluation of hydrocarbon preservation in marine carbonate rock areas:Taking lower association in central Sichuan Basin as an example[J].Journal of Chengdu University of Technology:Science&Technology Edition,2009,36(6):631-634.王国芝,刘树根.海相碳酸盐岩区油气保存条件的古流体地球化学评价---以四川盆地中部下组合为例[J].成都理工大学学报:自然科学版,2009,36(6):631-644.
[31]Liu Shugen,Sun Wei,Wang Guozhi,et al.Analysis of causes of oil and gas accumulation in superimposed Sichuan Basin of China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2013,40(5):481-497.刘树根,孙玮,王国芝,等.四川叠合盆地油气富集原因剖析[J].成都理工大学学报:自然科学版,2013,40(5):481-497.
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