四川盆地二叠系火山岩岩相与储层特征
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摘要
为了给四川盆地火山岩气藏下一步的勘探部署提供依据,综合利用钻井录井、分析化验、测井及地震等资料,在对该盆地二叠系火山岩分类的基础上,研究了不同类型火山岩的岩性特征、岩相特征与岩相分布、储层特征,并确定了控制火山岩储层发育的主要因素。研究结果表明:①该盆地火山岩可综合划分为火山熔岩、火山碎屑熔岩、火山碎屑岩及沉火山碎屑岩4大类,主要发育玄武岩、角砾熔岩、含凝灰角砾熔岩、凝灰岩和沉凝灰岩等岩石类型;②该盆地内大面积分布溢流相、喷溢相和火山沉积相等3种火山岩相类型,其中溢流相主要发育玄武岩,喷溢相主要发育火山碎屑熔岩,火山沉积相主要发育凝灰岩及沉凝灰岩等;③火山岩储层岩性主要为火山碎屑熔岩和玄武岩,其中火山碎屑熔岩主要发育脱玻化微孔、溶蚀孔,为中孔、低渗的孔隙型储层,玄武岩主要发育裂缝及溶孔,为基质孔隙度较低的孔隙—裂缝型储层;④火山岩储层控制因素主要为岩性、岩相、后期流体改造作用和构造作用,其中火山碎屑熔岩在快速冷凝的过程中脱玻化形成大量弥散状微孔,为后期进一步溶蚀增孔提供了有利条件,溶蚀等成岩作用及裂缝发育使储层物性变好。结论认为,四川盆地二叠系火山岩储层的平面展布主要受岩相控制,川西南部雅安—乐山—屏山地区主要发育孔隙—裂缝型玄武岩储层,成都—简阳—三台地区主要发育孔隙型火山碎屑熔岩储层。
In order to provide basis for further exploration and deployment of volcanic gas reservoirs in the Sichuan Basin, we classified Permian volcanic rocks in this basin using drilling, mud logging, assay, logging and seismic data comprehensively. Then, the lithological characteristics, lithofacies characteristics, lithofacies distribution and reservoir characteristics of different types of volcanic rocks were studied. Besides, the main factors controlling the development of volcanic reservoirs were determined. And the following research results were obtained. First, volcanic rocks in the Sichuan Basin can be comprehensively classified into 4 categories(i.e., volcanic lava, vocaniclastic lava, volcaniclastic rocks and sedimentary volcaniclastic rocks), and basalt, breccia lava, tuffaceous breccia lava, tuff, sedimentary tuff are mainly developed. Second, 3 types of volcanic lithofacies are extensively developed in the Sichuan Basin, including overflow facies, effusive facies and volcanic sedimentary facies. Overflow facies is mainly dominated by basalt, effusive facies is mainly composed of volcaniclastic lava, and volcanic sedimentary facies is mainly composed of tuff and sedimentary tuff. Third, volcanic reservoirs are lithologically composed of breccia lava and basalt. Breccia lava reservoirs are pore-type reservoirs of moderate porosity and low permeability with devitrified micropores and dissolution pores as main reservoir space. In basalt, fractures and dissolution pores are mainly developed, and they are porous-fractured reservoirs with lower matrix porosity. Fourth, the factors controlling volcanic reservoirs mainly include lithology, lithofacies, later fluid alteration and tectonism. Volcaniclastic lava is devitrified in the process of rapid condensation, and a great number of dispersion-shape micropores are formed to provide favorable conditions for further dissolution and pore enhancement in the later stage. Post-diagenesis effect(e.g. dissolution) and fracture development make the reservoir properties better. In conclusion,the areal distribution of volcanic reservoirs in the Sichuan Basin is mainly controlled by the lithofacies. Porous-fractured basalt reservoirs are mainly developed in the Ya'an–Leshan–Pingshan area in the southwestern Sichuan Basin, and pore-type vocaniclastic lava reservoirs are mainly developed in the Chengdu–Jianyang–Santai area.
In order to provide basis for further exploration and deployment of volcanic gas reservoirs in the Sichuan Basin, we classified Permian volcanic rocks in this basin using drilling, mud logging, assay, logging and seismic data comprehensively. Then, the lithological characteristics, lithofacies characteristics, lithofacies distribution and reservoir characteristics of different types of volcanic rocks were studied. Besides, the main factors controlling the development of volcanic reservoirs were determined. And the following research results were obtained. First, volcanic rocks in the Sichuan Basin can be comprehensively classified into 4 categories(i.e., volcanic lava, vocaniclastic lava, volcaniclastic rocks and sedimentary volcaniclastic rocks), and basalt, breccia lava, tuffaceous breccia lava, tuff, sedimentary tuff are mainly developed. Second, 3 types of volcanic lithofacies are extensively developed in the Sichuan Basin, including overflow facies, effusive facies and volcanic sedimentary facies. Overflow facies is mainly dominated by basalt, effusive facies is mainly composed of volcaniclastic lava, and volcanic sedimentary facies is mainly composed of tuff and sedimentary tuff. Third, volcanic reservoirs are lithologically composed of breccia lava and basalt. Breccia lava reservoirs are pore-type reservoirs of moderate porosity and low permeability with devitrified micropores and dissolution pores as main reservoir space. In basalt, fractures and dissolution pores are mainly developed, and they are porous-fractured reservoirs with lower matrix porosity. Fourth, the factors controlling volcanic reservoirs mainly include lithology, lithofacies, later fluid alteration and tectonism. Volcaniclastic lava is devitrified in the process of rapid condensation, and a great number of dispersion-shape micropores are formed to provide favorable conditions for further dissolution and pore enhancement in the later stage. Post-diagenesis effect(e.g. dissolution) and fracture development make the reservoir properties better. In conclusion,the areal distribution of volcanic reservoirs in the Sichuan Basin is mainly controlled by the lithofacies. Porous-fractured basalt reservoirs are mainly developed in the Ya'an–Leshan–Pingshan area in the southwestern Sichuan Basin, and pore-type vocaniclastic lava reservoirs are mainly developed in the Chengdu–Jianyang–Santai area.
引文
[1]田景春,林小兵,郭维,张翔,黄平辉.四川盆地二叠纪玄武岩喷发事件的油气地质意义[J].成都理工大学学报(自然科学版),2017,44(1):14-20.Tian Jingchun,Lin Xiaobing,Guo Wei,Zhang Xiang&Huang Pinghui.Geological significance of oil and gas in the Permian basalt eruption event in Sichuan Basin,China[J].Journal of Chengdu University of Technology(Science&Technology Edition),2017,44(1):14-20.
[2]杨毅,张本健,蒋德生,裴森奇,周子琰.四川盆地西南部上二叠统峨眉山玄武岩成藏模式初探[J].天然气工业,2010,30(5):46-49.Yang Yi,Zhang Benjian,Jiang Desheng,Pei Senqi&Zhou Ziyan.A preliminary study on hydrocarbon pooling patterns of the Upper Permian Emeishan basalts in southwestern Sichuan Basin[J].Natural Gas Industry,2010,30(5):46-49.
[3]魏杰.峨眉山玄武岩岩石学、岩石地球化学及其地球动力学意义[D].成都:成都理工大学,2018.Wei Jie.The petrology,rok geochemistry and geodynamic significance of the Emeishan basalt[D].Chengdu:Chengdu University of Technology,2018.
[4]徐义刚,钟孙霖.峨眉山大火成岩省:地幔柱活动的证据及其熔融条件[J].地球化学,2001,30(1):1-9.Xu Yigang&Zhong Sunlin.The Emeishan large igneous province:Evidence for mantle plume activity and melting conditions[J].Geochimica,2001,30(1):1-9.
[5]周志敏.四川盐源二叠纪玄武岩地质地球化学特征及成岩演化[D].成都:成都理工大学,2018.Zhou Zhimin.Geological and geochemical characteristics and diagenetic evolution of Permian basalts from Yanyuan,Sichuan province[D].Chengdu:Chengdu University of Technology,2018.
[6]李宏博.峨眉山大火成岩省地幔柱动力学:基性岩墙群、地球化学及沉积地层学证据[D].北京:中国地质大学(北京),2012.Li Hongbo.Dynamics of mantle plume in Emeishan large igneous province:Evidence of basic rock wall group,geochemistry and sedimentary stratigraphy[D].China University of Geosciences(Beijing),2012
[7]张招崇,王福生,郝艳丽.峨眉山大火成岩省中的苦橄岩:地幔柱活动证据[J].矿物岩石地球化学通报,2005,24(1):17-22.Zhang Zhaochong,Wang Fusheng&Hao Yanli.Picrites from the Emeishan large igneous province:Evidence for the mantle plume activity[J].Bulletin of Mineralogy,Petrology and Geochemistry,2005,24(1):17-22.
[8]王璞珺,陈树民,刘万洙,单玄龙,程日辉,张艳,等.松辽盆地火山岩相与火山岩储层的关系[J].石油与天然气地质,2003,24(1):18-23.Wang Pujun,Chen Shumin,Liu Wanzhu,Shan Xuanlong,Cheng Rihui,Zhang Yan,et al.Relationship between volcanic facies and volcanic reservoirs in Songliao Basin[J].Oil&Gas Geology,2003,24(1):18-23.
[9]王璞珺,缴洋洋,杨凯凯,张增宝,边伟华.准噶尔盆地火山岩分类研究与应用[J].吉林大学学报(地球科学版),2016,46(4):1056-1070.Wang Pujun,Jiao Yangyang,Yang Kaikai,Zhang Zengbao&Bian Weihua.Classification of volcanogenic successions and its application to volcanic reservoir exploration in the Junggar Basin,NW China[J].Journal of Jilin University(Earth Science Edition),2016,46(4):1056-1070.
[10]程黎鹿.峨眉山大火成岩省的岩浆运移、滞留、演化过程的岩石学和数值模拟研究[D].北京:中国地质大学(北京),2014.Cheng Lilu.Petrology and numerical simulation of magma migration,retention and evolution in the Emeishan large igneous province[D].Beijing:China University of Geosciences(Beijing),2014.
[11]时应敏,何登发,石胜群.松辽盆地长岭断陷东部营城组火山岩储层特征[J].石油实验地质,2011,33(2):171-176.Shi Yingmin,He Dengfa&Shi Shengqun.Characteristics of volcanic reservoir of Yingcheng Formation in East Changling Fault Depression,Songliao Basin[J].Petroleum Geology&Experiment,2011,33(2):171-176.
[12]陆建林,张玉明,徐宏节,赵德力.松辽盆地长岭断陷火山岩储层形成特征研究[J].石油实验地质,2009,31(5):441-448.Lu Jianlin,Zhang Yuming,Xu Hongjie&Zhao Deli.Studies of volcanic reservoir forming characteristics of Changling Faulted Depression,the Songliao Basin[J].Petroleum Geology&Experiment,2009,31(5):441-448.
[13]黄亮,彭军,周康,陈远建,柳军.火山岩储层形成机制研究综述[J].特种油气藏,2009,16(1):1-5.Huang Liang,Peng Jun,Zhou Kang,Chen Yuanjian&Liu Jun.An overview of the study on formation mechanism of volcanic reservoirs[J].Special Oil&Gas Reservoirs,2009,16(1):1-5.
[14]赵海玲,黄微,王成,狄永军,齐井顺,肖勇,等.火山岩中脱玻化孔及其对储层的贡献[J].石油与天然气地质,2009,30(1):47-58.Zhao Hailing,Huang Wei,Wang Cheng,Di Yongjun,Qi Jingshun,Xiao Yong,et al.Micropores from devitrification in volcanic rocks and their contribution to reservoirs[J].Oil&Gas Geology,2009,30(1):47-58.
[15]蒋裕强,谷一凡,李开鸿,李顺,罗明生,何冰.四川盆地中部中二叠统热液白云岩储渗空间类型及成因[J].天然气工业,2018,38(2):16-24.Jiang Yuqiang,Gu Yifan,Li Kaihong,Li Shun,Luo Mingsheng&He Bing.Space types and origins of hydrothermal dolomite reservoirs in the Middle Permian strata,Central Sichuan Basin[J].Natural Gas Industry,2018,38(2):16-24.
[16]任康绪,王小军,吴宝成,邓西里,穆剑东,刘畅.不同碱度火成岩溶蚀增孔差异性对比[J].石油学报,2015,36(7):799-808.Ren Kangxu,Wang Xiaojun,Wu Baocheng,Deng Xili,Mu Jiandong&Liu Chang.Comparation on differences of increasing porosity for different alkali contents igneous rocks[J].Acta Petrolei Sinica,2015,36(7):799-808.
[17]白莹,罗平,刘伟,翟秀芬,周川闽.微生物碳酸盐岩储层特征及主控因素--以塔里木盆地阿克苏地区下寒武统肖尔布拉克组上段为例[J].中国石油勘探,2018,23(4):95-106.Bai Ying,Luo Ping,Liu Wei,Zhai Xiufen&Zhou Chuanmin.Characteristics and main controlling factors of microbial carbonate reservoir:A case study of upper member of Lower Cambrian Xiaoerbulake Formation in Akesu area,Tarim Basin[J].China Petroleum Exploration,2018,23(4):95-106.
[18]冯仁蔚,王兴志,张帆,杨跃明,李跃刚,庞艳君,等.四川西南部周公山及邻区“峨眉山玄武岩”特征及储集性能研究[J].沉积学报,2008,26(6):913-924.Feng Renwei,Wang Xingzhi,Zhang Fan,Yang Yueming,Li Yuegang,Pang Yanjun,et al.The Study on reservoir property and characteristics of the Emeishan basalts of Zhougongshan and its neighbour area in the Southwest Sichuan[J].Acta Sedimentologica Sinica,2008,26(6):913-924.
[19]刘冉,霍飞,王鑫,杨涛,李熹微,陈柯童.普光气田下三叠统飞仙关组碳酸盐岩储层特征及主控因素分析[J].中国石油勘探,2017,22(6):34-46.Liu Ran,Huo Fei,Wang Xin,Yang Tao,Li Xiwei&Chen Ketong.Characteristics and main controlling factors of Lower Triassic Feixianguan Formation carbonate reservoir in Puguang gas field[J].China Petroleum Exploration,2017,22(6):34-46.
[20]王文才,李秀华.峨眉山地区“峨眉山玄武岩”顶部发现古风化壳[J].矿物岩石,1982,1(1):14.Wang Wencai&Li Xiuhua.Ancient weathering crust of the top of Emei mountain basalt in Emei areas,Sichuan[J].Journal of Mineralogy and Petrology,1982,1(1):14.
[21]王正瑛,李秀华,王文才,刘集银,刘爱玉.峨眉龙门洞地区峨眉山玄武岩顶部古风化壳[J].矿物岩石,1982,1(3):56-64.Wang Zhengying,Li Xiuhua,Wang Wencai,Liu Jiyin&Liu Aiyu.Ancient weathering crust of the top of Emei mountain basalt in Emei Longmendong areas,Sichuan[J].Journal of Mineralogy and Petrology,1982,1(3):56-64.
[22]侯明才,王文楷,张本健,王维,李秀华,邓敏,等.四川周公山-汉王场地区峨眉山玄武岩中流体类型及活动期次[J].岩石学报,2013,29(8):2709-2718.Hou Mingcai,Wang Wenkai,Zhang Benjian,Wang Wei,Li Xiuhua,Deng Min,et al.Fluid types and activities of Emeishan basalt in Zhougong mountain-Hanwang field of Sichuan province[J].Acta Petrologica Sinica,2013,29(8):2709-2718.
[23]刘丛强,黄智龙,李和平,苏根利.地幔流体及其成矿作用[J].地学前缘,2001,8(4):231-243.Liu Congqiang,Huang Zhilong,Li Heping&Su Genli.The geofluid in the mantle and its role in ore-forming processes[J].Earth Science Frontiers,2001,8(4):231-243.
[24]汤艳杰,贾建业,谢先德.粘土矿物的环境意义[J].地学前缘,2002,9(2):337-344.Tang Yanjie,Jia Jianye&Xie Xiande.Environment significance of clay minerals[J].Earth Science Frontiers,2002,9(2):337-344.
[25]任帮政.峨眉山玄武岩斜坡残积土中粘土矿物的形成机制研究[D].昆明:昆明理工大学,2014.Ren Bangzheng.The formation mechanism of clay minerals in residual soil of Emeishan Basalt Slope[D].Kunming:Kunming University of Science and Technology,2014.
[26]邵英梅,冯子辉.徐家围子断陷营城组火山岩岩石学及地球化学特征[J].大庆石油地质与开发,2007,26(4):27-30.Shao Yingmei&Feng Zihui.Petrologic and geochemical characteristics of volcanic rock of Yingcheng Formation in Xujiaweizi fault depression[J].Petroleum Geology&Oilfield Development in Daqing,2007,26(4):27-30.
[27]柳双权,张顺存,戴龙,矫睿,鲁新川,史基安,等.准噶尔盆地石炭系火山岩优质储层特征及主控因素[J].兰州大学学报(自然科学版),2014,50(6):786-794.Liu Shuangquan,Zhang Shuncun,Dai Long,Jiao Rui,Lu Xinchuan,Shi Ji'an,et al.Characteristics and main controlling factors of high quality carboniferous volcanic reservoirs in Junggar Basin[J].Journal of Lanzhou University(Natural Sciences),2014,50(6):786-794.
[2]杨毅,张本健,蒋德生,裴森奇,周子琰.四川盆地西南部上二叠统峨眉山玄武岩成藏模式初探[J].天然气工业,2010,30(5):46-49.Yang Yi,Zhang Benjian,Jiang Desheng,Pei Senqi&Zhou Ziyan.A preliminary study on hydrocarbon pooling patterns of the Upper Permian Emeishan basalts in southwestern Sichuan Basin[J].Natural Gas Industry,2010,30(5):46-49.
[3]魏杰.峨眉山玄武岩岩石学、岩石地球化学及其地球动力学意义[D].成都:成都理工大学,2018.Wei Jie.The petrology,rok geochemistry and geodynamic significance of the Emeishan basalt[D].Chengdu:Chengdu University of Technology,2018.
[4]徐义刚,钟孙霖.峨眉山大火成岩省:地幔柱活动的证据及其熔融条件[J].地球化学,2001,30(1):1-9.Xu Yigang&Zhong Sunlin.The Emeishan large igneous province:Evidence for mantle plume activity and melting conditions[J].Geochimica,2001,30(1):1-9.
[5]周志敏.四川盐源二叠纪玄武岩地质地球化学特征及成岩演化[D].成都:成都理工大学,2018.Zhou Zhimin.Geological and geochemical characteristics and diagenetic evolution of Permian basalts from Yanyuan,Sichuan province[D].Chengdu:Chengdu University of Technology,2018.
[6]李宏博.峨眉山大火成岩省地幔柱动力学:基性岩墙群、地球化学及沉积地层学证据[D].北京:中国地质大学(北京),2012.Li Hongbo.Dynamics of mantle plume in Emeishan large igneous province:Evidence of basic rock wall group,geochemistry and sedimentary stratigraphy[D].China University of Geosciences(Beijing),2012
[7]张招崇,王福生,郝艳丽.峨眉山大火成岩省中的苦橄岩:地幔柱活动证据[J].矿物岩石地球化学通报,2005,24(1):17-22.Zhang Zhaochong,Wang Fusheng&Hao Yanli.Picrites from the Emeishan large igneous province:Evidence for the mantle plume activity[J].Bulletin of Mineralogy,Petrology and Geochemistry,2005,24(1):17-22.
[8]王璞珺,陈树民,刘万洙,单玄龙,程日辉,张艳,等.松辽盆地火山岩相与火山岩储层的关系[J].石油与天然气地质,2003,24(1):18-23.Wang Pujun,Chen Shumin,Liu Wanzhu,Shan Xuanlong,Cheng Rihui,Zhang Yan,et al.Relationship between volcanic facies and volcanic reservoirs in Songliao Basin[J].Oil&Gas Geology,2003,24(1):18-23.
[9]王璞珺,缴洋洋,杨凯凯,张增宝,边伟华.准噶尔盆地火山岩分类研究与应用[J].吉林大学学报(地球科学版),2016,46(4):1056-1070.Wang Pujun,Jiao Yangyang,Yang Kaikai,Zhang Zengbao&Bian Weihua.Classification of volcanogenic successions and its application to volcanic reservoir exploration in the Junggar Basin,NW China[J].Journal of Jilin University(Earth Science Edition),2016,46(4):1056-1070.
[10]程黎鹿.峨眉山大火成岩省的岩浆运移、滞留、演化过程的岩石学和数值模拟研究[D].北京:中国地质大学(北京),2014.Cheng Lilu.Petrology and numerical simulation of magma migration,retention and evolution in the Emeishan large igneous province[D].Beijing:China University of Geosciences(Beijing),2014.
[11]时应敏,何登发,石胜群.松辽盆地长岭断陷东部营城组火山岩储层特征[J].石油实验地质,2011,33(2):171-176.Shi Yingmin,He Dengfa&Shi Shengqun.Characteristics of volcanic reservoir of Yingcheng Formation in East Changling Fault Depression,Songliao Basin[J].Petroleum Geology&Experiment,2011,33(2):171-176.
[12]陆建林,张玉明,徐宏节,赵德力.松辽盆地长岭断陷火山岩储层形成特征研究[J].石油实验地质,2009,31(5):441-448.Lu Jianlin,Zhang Yuming,Xu Hongjie&Zhao Deli.Studies of volcanic reservoir forming characteristics of Changling Faulted Depression,the Songliao Basin[J].Petroleum Geology&Experiment,2009,31(5):441-448.
[13]黄亮,彭军,周康,陈远建,柳军.火山岩储层形成机制研究综述[J].特种油气藏,2009,16(1):1-5.Huang Liang,Peng Jun,Zhou Kang,Chen Yuanjian&Liu Jun.An overview of the study on formation mechanism of volcanic reservoirs[J].Special Oil&Gas Reservoirs,2009,16(1):1-5.
[14]赵海玲,黄微,王成,狄永军,齐井顺,肖勇,等.火山岩中脱玻化孔及其对储层的贡献[J].石油与天然气地质,2009,30(1):47-58.Zhao Hailing,Huang Wei,Wang Cheng,Di Yongjun,Qi Jingshun,Xiao Yong,et al.Micropores from devitrification in volcanic rocks and their contribution to reservoirs[J].Oil&Gas Geology,2009,30(1):47-58.
[15]蒋裕强,谷一凡,李开鸿,李顺,罗明生,何冰.四川盆地中部中二叠统热液白云岩储渗空间类型及成因[J].天然气工业,2018,38(2):16-24.Jiang Yuqiang,Gu Yifan,Li Kaihong,Li Shun,Luo Mingsheng&He Bing.Space types and origins of hydrothermal dolomite reservoirs in the Middle Permian strata,Central Sichuan Basin[J].Natural Gas Industry,2018,38(2):16-24.
[16]任康绪,王小军,吴宝成,邓西里,穆剑东,刘畅.不同碱度火成岩溶蚀增孔差异性对比[J].石油学报,2015,36(7):799-808.Ren Kangxu,Wang Xiaojun,Wu Baocheng,Deng Xili,Mu Jiandong&Liu Chang.Comparation on differences of increasing porosity for different alkali contents igneous rocks[J].Acta Petrolei Sinica,2015,36(7):799-808.
[17]白莹,罗平,刘伟,翟秀芬,周川闽.微生物碳酸盐岩储层特征及主控因素--以塔里木盆地阿克苏地区下寒武统肖尔布拉克组上段为例[J].中国石油勘探,2018,23(4):95-106.Bai Ying,Luo Ping,Liu Wei,Zhai Xiufen&Zhou Chuanmin.Characteristics and main controlling factors of microbial carbonate reservoir:A case study of upper member of Lower Cambrian Xiaoerbulake Formation in Akesu area,Tarim Basin[J].China Petroleum Exploration,2018,23(4):95-106.
[18]冯仁蔚,王兴志,张帆,杨跃明,李跃刚,庞艳君,等.四川西南部周公山及邻区“峨眉山玄武岩”特征及储集性能研究[J].沉积学报,2008,26(6):913-924.Feng Renwei,Wang Xingzhi,Zhang Fan,Yang Yueming,Li Yuegang,Pang Yanjun,et al.The Study on reservoir property and characteristics of the Emeishan basalts of Zhougongshan and its neighbour area in the Southwest Sichuan[J].Acta Sedimentologica Sinica,2008,26(6):913-924.
[19]刘冉,霍飞,王鑫,杨涛,李熹微,陈柯童.普光气田下三叠统飞仙关组碳酸盐岩储层特征及主控因素分析[J].中国石油勘探,2017,22(6):34-46.Liu Ran,Huo Fei,Wang Xin,Yang Tao,Li Xiwei&Chen Ketong.Characteristics and main controlling factors of Lower Triassic Feixianguan Formation carbonate reservoir in Puguang gas field[J].China Petroleum Exploration,2017,22(6):34-46.
[20]王文才,李秀华.峨眉山地区“峨眉山玄武岩”顶部发现古风化壳[J].矿物岩石,1982,1(1):14.Wang Wencai&Li Xiuhua.Ancient weathering crust of the top of Emei mountain basalt in Emei areas,Sichuan[J].Journal of Mineralogy and Petrology,1982,1(1):14.
[21]王正瑛,李秀华,王文才,刘集银,刘爱玉.峨眉龙门洞地区峨眉山玄武岩顶部古风化壳[J].矿物岩石,1982,1(3):56-64.Wang Zhengying,Li Xiuhua,Wang Wencai,Liu Jiyin&Liu Aiyu.Ancient weathering crust of the top of Emei mountain basalt in Emei Longmendong areas,Sichuan[J].Journal of Mineralogy and Petrology,1982,1(3):56-64.
[22]侯明才,王文楷,张本健,王维,李秀华,邓敏,等.四川周公山-汉王场地区峨眉山玄武岩中流体类型及活动期次[J].岩石学报,2013,29(8):2709-2718.Hou Mingcai,Wang Wenkai,Zhang Benjian,Wang Wei,Li Xiuhua,Deng Min,et al.Fluid types and activities of Emeishan basalt in Zhougong mountain-Hanwang field of Sichuan province[J].Acta Petrologica Sinica,2013,29(8):2709-2718.
[23]刘丛强,黄智龙,李和平,苏根利.地幔流体及其成矿作用[J].地学前缘,2001,8(4):231-243.Liu Congqiang,Huang Zhilong,Li Heping&Su Genli.The geofluid in the mantle and its role in ore-forming processes[J].Earth Science Frontiers,2001,8(4):231-243.
[24]汤艳杰,贾建业,谢先德.粘土矿物的环境意义[J].地学前缘,2002,9(2):337-344.Tang Yanjie,Jia Jianye&Xie Xiande.Environment significance of clay minerals[J].Earth Science Frontiers,2002,9(2):337-344.
[25]任帮政.峨眉山玄武岩斜坡残积土中粘土矿物的形成机制研究[D].昆明:昆明理工大学,2014.Ren Bangzheng.The formation mechanism of clay minerals in residual soil of Emeishan Basalt Slope[D].Kunming:Kunming University of Science and Technology,2014.
[26]邵英梅,冯子辉.徐家围子断陷营城组火山岩岩石学及地球化学特征[J].大庆石油地质与开发,2007,26(4):27-30.Shao Yingmei&Feng Zihui.Petrologic and geochemical characteristics of volcanic rock of Yingcheng Formation in Xujiaweizi fault depression[J].Petroleum Geology&Oilfield Development in Daqing,2007,26(4):27-30.
[27]柳双权,张顺存,戴龙,矫睿,鲁新川,史基安,等.准噶尔盆地石炭系火山岩优质储层特征及主控因素[J].兰州大学学报(自然科学版),2014,50(6):786-794.Liu Shuangquan,Zhang Shuncun,Dai Long,Jiao Rui,Lu Xinchuan,Shi Ji'an,et al.Characteristics and main controlling factors of high quality carboniferous volcanic reservoirs in Junggar Basin[J].Journal of Lanzhou University(Natural Sciences),2014,50(6):786-794.