徐深气田徐东地区营城组一段火山岩储层岩相特征
|
摘要
在火山岩岩石类型划分基础上,结合地质、测井和地震资料综合分析,识别火山岩体。在此基础上将研究区目的层火山岩相划分为爆发相、溢流相等5种类型和溅落亚相、空落亚相等16种亚相类型。通过单井、剖面地震相、平面地震相和火山岩相特征分析,认为火山口对火山岩体具有重要的控制作用,在火山岩体的不同部位发育不同的火山岩相类型,不同类型的火山岩相展布又控制着火山岩气藏储层的分布特征。研究区储层主要发育于爆发相和溢流相中,少数发育于其他相带。爆发相溅落亚相、空落亚相,侵出相外带亚相、中带亚相,溢流相下部亚相、顶部亚相、上部亚相,火山通道相的火山颈亚相等为优质储集体发育部位。
Based on volcanic rock types,we identified the volcanic bodies,in combination with geological background,logging and seismic data.Volcanic lithofacies for selective layer were classified into 5 facies,such as eruptive and effusive,etc.and 16 sub-facies,like as landing,etc.By means of seismic facies and volcanic lithofacies for single well,cut and plane sections,we found out that crater distribution constrained development of volcanic body,associated with different volcanic facies in the different positions of volcanic body.The space of volcanic facies controlled the high quality reservoir of volcanic rock.Most of high-quality reservoir was mainly distributed in the areas of eruptive and effusive facies,and few did in other facies.The high-quality reservoir was developed in the areas of landing and air falling sub-facies in eruptive facies,outer and middle extrusive sub-facies in extrusive facies,lower,upper and top sub-facies in overflow facies,and volcanic neck sub-facies in volcanic channels facies.
Based on volcanic rock types,we identified the volcanic bodies,in combination with geological background,logging and seismic data.Volcanic lithofacies for selective layer were classified into 5 facies,such as eruptive and effusive,etc.and 16 sub-facies,like as landing,etc.By means of seismic facies and volcanic lithofacies for single well,cut and plane sections,we found out that crater distribution constrained development of volcanic body,associated with different volcanic facies in the different positions of volcanic body.The space of volcanic facies controlled the high quality reservoir of volcanic rock.Most of high-quality reservoir was mainly distributed in the areas of eruptive and effusive facies,and few did in other facies.The high-quality reservoir was developed in the areas of landing and air falling sub-facies in eruptive facies,outer and middle extrusive sub-facies in extrusive facies,lower,upper and top sub-facies in overflow facies,and volcanic neck sub-facies in volcanic channels facies.
引文
[1]Zhang Shuncun,Wang Ling,Shi Xinpu,et al.Physical charac-teristics and their relations to logging of the Carboniferousvolcanic reservoirs in Luxi area,Junggar basin[J].NaturalGas Geoscience,2008,19(2):198-203.[张顺存,王凌,石新璞,等.准噶尔盆地腹部陆西地区石炭系火山岩储层的物性特征及其与电性的关系[J].天然气地球科学,2008,19(2):198-203.]
[2]Wang Dezi,Zhou Xinmin.Volcanic Rock Lithology[M].Bei-jing:Science Press,1982.[王德滋,周新民.火山岩岩石学[M].北京:科学出版社,1982.]
[3]Hong Tang,Ji Hancheng.Incorporation of Spatial Charactersinto Volcanic Facies and Favorable Reservoir Prediction[R].SPE 90847,2004:1-11.
[4]Wang Pujun,Feng Zhiqiang.Basin Volcanic Lithology,Litho-facies,Reservoir,Gas Accumulation and Prospecting[M].Bei-jing:Science Press,2008.[王璞?,冯志强.盆地火山岩岩性、岩相、储层、气藏、勘探[M].北京:科学出版社,2008.]
[5]Zhao Chenlin,Liu Menghui,Hu Aimei,et al.Special Petrole-um Reservoir[M].Beijing:Petroleum Insustry Press,1997.[赵澄林,刘孟慧,胡爱梅,等.特殊油气储层[M].北京:石油工业出版社,1997.]
[6]Wang Ling,Sun Xiping,Zhang Yan,et al.Volcanic massif ge-netic mechanism and volcanic facies controlled by deep zonefaulted systems in Songliao basin:A case in Xushen area[J].Natural Gas Geoscience,2007,18(3):389-393.[王玲,孙夕平,张研,等.松辽盆地深层断裂体系对火山岩成因和火山岩相带的控制:以徐深地区为例[J].天然气地球科学,2007,18(3):389-393.]
[7]Wu Heyong,Yang Fengping,Ren Yanguang,et al.Gas Reser-voir Evaluated of Xushen-1 Well Area of Xujiaweizi Depres-sion in the North of Songliao Basin[M].Beijing:Petroleun In-dustry Press,2002.[吴河勇,杨峰平,任延广,等.松辽盆地北部徐家围子断陷徐深1井区气藏评价[M].北京:石油工业出版社,2002.]
[8]Shu Ping,Ding Rixin,Qu Yanming,et al.Lithologic and litho-facies patterns of volcanic reservoir in Xushen gas field[J].Natural Gas Industry,2007,27(8):23-27.[舒萍,丁日新,曲延明,等.徐深气田火山岩储层岩性岩相模式[J].天然气工业,2007,27(8):23-27.]
[9]Wang Yongjun,Yan Lin,Ran Qiquan,et al.Lithology distin-guishing technology research of deep layer volcanic gas reser-voir in Xushen gas field[J].Journal of Southwest PetroleumUniversity,2007,29(2):78-81.[王拥军,闫林,冉启全,等.兴城气田深层火山岩气藏岩性识别技术研究[J].西南石油大学学报,2007,29(2):78-81.]
[10]Yan Lin,Hu Yongle,Ran Qiquan,et al.Volcanic characteris-tics and eruption models of Yingcheng Formation No.1 Mem-ber in Xingcheng area,Xujiaweizi fault-depression of Songliaobasin[J].Natural Gas Geoscience,2008,19(6):821-825.[闫林,胡永乐,冉启全,等.松辽盆地徐家围子断陷兴城地区营城组一段火山岩特征及火山喷发模式[J].天然气地球科学,2008,19(6):821-825.]
[11]Wang Zhengku,Ou Chenghua,Li Fengxia.Study on the li-thology discrimination methods for volcanic reservoirs[J].World Well Logging Technology,2007,22(1):8-11.[王郑库,欧成华,李凤霞.火山岩储层岩性识别方法研究[J].国外测井技术,2007,22(1):8-11.]
[12]Sun Yuanhui,Shen Pingping,Ruan Baotao,et al.Lithologicand storage-permeation characteristics of Changshen 1 volcan-ic gas reservoirs in Jilin[J].Natural Gas Geoscience,2008,19(5):630-633.[孙圆辉,沈平平,阮宝涛,等.松辽盆地长岭断陷长深1号气田火山岩岩性及储渗特征研究[J].天然气地球科学,2008,19(5):630-633.]
[13]Li Zubing,Luo Minggao,Wang Jianwei,et al.Research onmethods of identifying volcanic rocks:An example from Sha-hejie Group in 5th structure,Nanpu[J].Natural Gas Geosci-ence,2009,20(1):113-118.[李祖兵,罗明高,王建伟,等.利用测井资料识别火山岩岩性的方法探讨——以南堡5号构造沙河街组岩性圈闭为例[J].天然气地球科学,2009,20(1):113-118.]
[14]Guo Zhenhua,Wang Pujun,Yin Changhai,et al.Relationshipbetween lithofacies and of the logging facies of the volcanicreservoir rocks in Songliao basin[J].Journal of Jilin Universi-ty:Earth Science Edition,2006,36(2):207-214.[郭振华,王璞?,印长海,等.松辽盆地北部火山岩岩相与测井相关系研究[J].吉林大学学报:地球科学版,2006,36(2):207-214.]
[15]Yu Jing,Liu Dameng,Wen Ruixia,et al.Identifying volcaniclithofacies of Yingcheng Formatiom by seismic attributes inthe Anda fault depression of Songliao basin[J].Chinese Jour-nal of Geology,2009,44(2):595-604.[于晶,刘大锰,文瑞霞,等.松辽盆地北部安达断陷营城组火山岩岩相的地震识别[J].地质科学,2009,44(2):595-604.]
[2]Wang Dezi,Zhou Xinmin.Volcanic Rock Lithology[M].Bei-jing:Science Press,1982.[王德滋,周新民.火山岩岩石学[M].北京:科学出版社,1982.]
[3]Hong Tang,Ji Hancheng.Incorporation of Spatial Charactersinto Volcanic Facies and Favorable Reservoir Prediction[R].SPE 90847,2004:1-11.
[4]Wang Pujun,Feng Zhiqiang.Basin Volcanic Lithology,Litho-facies,Reservoir,Gas Accumulation and Prospecting[M].Bei-jing:Science Press,2008.[王璞?,冯志强.盆地火山岩岩性、岩相、储层、气藏、勘探[M].北京:科学出版社,2008.]
[5]Zhao Chenlin,Liu Menghui,Hu Aimei,et al.Special Petrole-um Reservoir[M].Beijing:Petroleum Insustry Press,1997.[赵澄林,刘孟慧,胡爱梅,等.特殊油气储层[M].北京:石油工业出版社,1997.]
[6]Wang Ling,Sun Xiping,Zhang Yan,et al.Volcanic massif ge-netic mechanism and volcanic facies controlled by deep zonefaulted systems in Songliao basin:A case in Xushen area[J].Natural Gas Geoscience,2007,18(3):389-393.[王玲,孙夕平,张研,等.松辽盆地深层断裂体系对火山岩成因和火山岩相带的控制:以徐深地区为例[J].天然气地球科学,2007,18(3):389-393.]
[7]Wu Heyong,Yang Fengping,Ren Yanguang,et al.Gas Reser-voir Evaluated of Xushen-1 Well Area of Xujiaweizi Depres-sion in the North of Songliao Basin[M].Beijing:Petroleun In-dustry Press,2002.[吴河勇,杨峰平,任延广,等.松辽盆地北部徐家围子断陷徐深1井区气藏评价[M].北京:石油工业出版社,2002.]
[8]Shu Ping,Ding Rixin,Qu Yanming,et al.Lithologic and litho-facies patterns of volcanic reservoir in Xushen gas field[J].Natural Gas Industry,2007,27(8):23-27.[舒萍,丁日新,曲延明,等.徐深气田火山岩储层岩性岩相模式[J].天然气工业,2007,27(8):23-27.]
[9]Wang Yongjun,Yan Lin,Ran Qiquan,et al.Lithology distin-guishing technology research of deep layer volcanic gas reser-voir in Xushen gas field[J].Journal of Southwest PetroleumUniversity,2007,29(2):78-81.[王拥军,闫林,冉启全,等.兴城气田深层火山岩气藏岩性识别技术研究[J].西南石油大学学报,2007,29(2):78-81.]
[10]Yan Lin,Hu Yongle,Ran Qiquan,et al.Volcanic characteris-tics and eruption models of Yingcheng Formation No.1 Mem-ber in Xingcheng area,Xujiaweizi fault-depression of Songliaobasin[J].Natural Gas Geoscience,2008,19(6):821-825.[闫林,胡永乐,冉启全,等.松辽盆地徐家围子断陷兴城地区营城组一段火山岩特征及火山喷发模式[J].天然气地球科学,2008,19(6):821-825.]
[11]Wang Zhengku,Ou Chenghua,Li Fengxia.Study on the li-thology discrimination methods for volcanic reservoirs[J].World Well Logging Technology,2007,22(1):8-11.[王郑库,欧成华,李凤霞.火山岩储层岩性识别方法研究[J].国外测井技术,2007,22(1):8-11.]
[12]Sun Yuanhui,Shen Pingping,Ruan Baotao,et al.Lithologicand storage-permeation characteristics of Changshen 1 volcan-ic gas reservoirs in Jilin[J].Natural Gas Geoscience,2008,19(5):630-633.[孙圆辉,沈平平,阮宝涛,等.松辽盆地长岭断陷长深1号气田火山岩岩性及储渗特征研究[J].天然气地球科学,2008,19(5):630-633.]
[13]Li Zubing,Luo Minggao,Wang Jianwei,et al.Research onmethods of identifying volcanic rocks:An example from Sha-hejie Group in 5th structure,Nanpu[J].Natural Gas Geosci-ence,2009,20(1):113-118.[李祖兵,罗明高,王建伟,等.利用测井资料识别火山岩岩性的方法探讨——以南堡5号构造沙河街组岩性圈闭为例[J].天然气地球科学,2009,20(1):113-118.]
[14]Guo Zhenhua,Wang Pujun,Yin Changhai,et al.Relationshipbetween lithofacies and of the logging facies of the volcanicreservoir rocks in Songliao basin[J].Journal of Jilin Universi-ty:Earth Science Edition,2006,36(2):207-214.[郭振华,王璞?,印长海,等.松辽盆地北部火山岩岩相与测井相关系研究[J].吉林大学学报:地球科学版,2006,36(2):207-214.]
[15]Yu Jing,Liu Dameng,Wen Ruixia,et al.Identifying volcaniclithofacies of Yingcheng Formatiom by seismic attributes inthe Anda fault depression of Songliao basin[J].Chinese Jour-nal of Geology,2009,44(2):595-604.[于晶,刘大锰,文瑞霞,等.松辽盆地北部安达断陷营城组火山岩岩相的地震识别[J].地质科学,2009,44(2):595-604.]
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心