天然气地球科学

• 天然气地质学 • 上一篇    下一篇

塔里木盆地英买35井区志留系储层石英增生机理及意义

刘永福,程明,孙琦,秦红,李洁   

  1. 中国石油塔里木油田分公司勘探开发研究院,新疆 库尔勒 841000
  • 收稿日期:2015-12-16 修回日期:2016-03-15 出版日期:2016-10-10 发布日期:2016-10-10
  • 作者简介:刘永福(1979-),男,山东威海人,高级工程师,主要从事沉积储层与石油地质研究.E-mail:liuyongf-tlm@petrochina.com.cn.
  • 基金资助:
    国家重大科技专项“塔里木盆地岩性地层油气藏富集区带、目标优选与勘探技术应用”(编号:2011ZX5001-002-003)资助.

Mechanism and its significance of quartz overgrowth in Silurian reservoir,Yingmai 35 Well area,Tarim Basin

Liu Yong-fu,Cheng Ming,Sun Qi,Qin Hong,Li Jie   

  1. Exploration & Development Research Institute,PetroChina Tarim Oilfield Company,Korla 841000,China
  • Received:2015-12-16 Revised:2016-03-15 Online:2016-10-10 Published:2016-10-10

摘要: 在英买35井区志留系柯坪塔格组上段,针对致密海相石英砂岩储层的成因,结合薄片、包裹体测温、伊利石测年、阴极发光等资料,认为石英砂岩存在4期主要的石英增生:①泥盆纪、石炭纪,来源于寒武系硅质生物遗骸中的硅质增生;②二叠纪火山喷发,来源于寒武系、奥陶系、志留系的硅质大量增生;③三叠纪、侏罗纪地层暴露剥蚀,来源于二叠系凝灰岩的硅质增生;④白垩纪至今地层快速沉降深埋,志留系成岩活动加剧,硅质析出增生。二叠系火成岩喷发提供了石英增生的动力与物源。毗邻二叠系火成岩侵入体的志留系砂岩储层存在热接触变质带和致密胶结带。

关键词: 石英砂岩, 增生, 火成岩, 储层, 志留系, 英买35井区

Abstract: Aiming at tight reservoir in marine quartz sandstone,combined with thin section,inclusion temperature,illite dating,cathodoluminescence,four stage quartz overgrowths were recognized in quartz sandstone,upper member of Kepingtage Formation,Silurian of Yingmai 35 Well area.(1)Quartz overgrowth whose silicon came from Cambrian siliceous biological remains in Devonian-Carboniferous;(2)Massive quartz overgrowth whose silicon came from Cambrian-Ordovician-Silurian formation during Permian volcanic eruption;(3)Quartz overgrowth whose silicon came from Permian volcanic tuff exposed and denuded during Triassic-Jurassic;(4)Quartz overgrowth because of Silurian Formation active diagenesis due to formation's fast sinking and deep burying,which happened from Cretaceous to present.Eruption of Permian igneous provided dynamic power and provenance for quartz overgrowth.Silurian sandstone formation included thermal contact aureole and dense cement zone,which was adjacent to Permian intrusive igneous rock.

Key words: Quartz sandstone, Overgrowth, Igneous, Reservoir, Silurian, Yingmai 35 Well area

中图分类号: 

  • TE122.2

[1]Guan Wensheng,Zha Ming,Zhang Chao,et al.Quantitative  evaluation of fault sealing with improving SGR method:A case study of Well Yingmai-34 area in Tabei Uplift,Tarim Basin[J].Xinjiang Petroleum Geology,2015,36(2):218-221.[管文胜,查明,张超,等.利用改进的SGR方法定量评价断层圈闭封堵性[J].新疆石油地质,2015,36(2):218-221.]
[2]Xiao Chengwen,Xin Yi,Gao Jinfa,et al.Log evaluation of epimetamorphic sandstone reservoirs with low-porosity and fractures in Silurian in north Tarim Basin[J].Well Logging Technology,2008,32(6):529-533.[肖承文,信毅,高进发,等.塔北志留系浅变质低孔隙度裂缝性砂岩储层测井评价[J].测井技术,2008,32(6):529-533.]
[3]Li Yusheng,Xie Chuanli,Deng Xingliang,et al.Reservoir characteristics and controlling factors of Silurian Kepingtage Formation in YM34 and YM35 Well blocks[J].Geology In China,2009,36(5):1087-1098.[李玉胜,谢传礼,邓兴梁,等.英买34、35井区志留系柯坪塔格组储层特征及其控制因素[J].中国地质,2009,36(5):1087-1098.]
[4]Zhang Ronghu,Zhang Huiliang,Zhou Chenguang,et al.Techonic compression and volcanic hydrothermal reconstruction effects of Silurian sandstone reservoirs in Yingmaili area[J].Acta Sedimentologica Sinica,2014,32(5):901-911.[张荣虎,张惠良,周晨光,等.塔里木盆地英买力地区志留系储层构造挤压及火山热液改造效应[J].沉积学报,2014,32(5):901-911.][JP]
[5]Guan Junfang.The two growth of quartz in sandstone of Permain system at Zhoukou Depression and Tongxu Uplift[J].Journal of North China Institute of Water Conservancy and Hydroelectric Power,2000,21(2):41-45.[管俊芳.周口拗陷和通许隆起二叠纪砂岩中石英的二次增生[J].华北水利水电学院学报,2000,21(2):41-45.]
[6]Chen Lihua,Guo Shunling,Wang Yanqi.Atlas of Chinese Petroleum Reservoir Micro-fluorescence and Cathodoluminescence of the Authigenic Mineral[M].Bejing:Petroleum Industry Press,1994:3-7.[陈丽华,郭舜玲,王衍琦.中国油气储层研究图集(第五卷)自生矿物显微荧光阴极发光[M].北京:石油工业出版社,1994:3-7.]
[7]Liu Xiang,Ding Xiong,Yang Jiajing,et al.Quantitative analysis of diagenesis and porosity evolution of reservoirs in the 2nd member of Xujiahe Formation of Hechuan Gasfield[J].Journal of Oil and Gas Technology:J.JPI,2013,35(3):20-25.[刘翔,丁熊,杨家静,等.合川气田须二段储层成岩与孔隙演化定量分析[J].石油天然气学报:江汉石油学院学报,2013,35(3):20-25.]
[8]Wu Xuechao,Tang Jun,Reng Laiyi.Diagenetic facies and high-quality reservoir study of Shanxi-2 member in Jingbian Gasfield,Ordos Basin[J].Natural Gas Geoscience,2012,23(6):1004- 1010.[吴雪超,汤军,任来义,等.鄂尔多斯盆地延长天然气探区山西组山2段成岩相及优质储层研究[J].天然气地球科学,2012,26(6):1004-1010.]
[9]Fei Weihong,Li Zhong,Sun Haishan.Quartz overgrowths and their reflecting fluid flow in Qiaokou- Baimiao region,Dongpu Depression[J].Chinese Journal of Geology,2001,36(2):152-163.[费卫红,李忠,孙海山.东濮凹陷桥口-白庙地区砂岩石英增生及其对流体活动的反映[J].地质科学,2001,36(2):152-163.]
[10]Wang Jing,Zhao Yanchao,Liu Kun,et al.Superimposing controls of acidic and alkaline dissolutions on sandstone reservoir quality of the Paleozoic Xiashihezi and Shanxi Formations in Tabamiao area,Ordos Basin[J].Earth Science:Journal of China University of Geosciences,2006,31(2):221-228.[王京,赵彦超,刘琨,等.鄂尔多斯盆地塔巴庙地区上古生界砂岩储层“酸性+碱性”叠加溶蚀作用与储层质量主控因素[J].地球科学:中国地质大学学报,2006,31(2):221-228.]
[11][KG*6/7]Li Shujun.Reservoir characteristics of Chang-6 oil-bearing formation in Houshi Tract,Ansai Oilfield[J].Journal of Xi’an Petroleum University:Natural Science Edition,1998,13(4):5-9.[李恕军.安塞油田侯市地区长6油层储层特征[J].西安石油学院学报,1998,13(4):5-9.]
[12]Zhang Jinliang,Du Guilin.Diagenesis of Silurian asphalt sandstones in Tazhong area and its impact on reservoir quality[J].Journal of Mineralogy and Petrology,2006,26(3):85-93.[张金亮,杜桂林.塔中地区志留系沥青砂岩成岩作用及其对储层性质的影响[J].矿物岩石,2006,26(3):85-93.]
[13]Jutta Weber,Werner Ricken.Quartz cementation and related sedimentary architecture of the Triassic solling formation,Reinhardswald Basin,Germany[J].Sedimentary Geology,2005,175:459-477.
[14]Ren Kangxu,Pan Wenqing,Gao Hongliang,et al.Reservoir characteristics and play target of igneous rocks,western Tabei Uplift[J].Natural Gas Exploration & Development,2007,30(2):1-4.[任康绪,潘文庆,高宏亮,等.塔北隆起西部火成岩储层特征及其勘探方向[J].天然气勘探与开发,2007,30(2):1-4.][JP]
[15]Zhang Youyu,Luo Xiuquan.K-Ar dating of authigenic illites and the hydrocarbon accumulation history of the Silurian bituminous sandstone reservoirs in the Yingmaili area,Tarim Basin[J].Petroleum Exploration and Development,2011,38(2):203-210.[张有瑜,罗修泉.英买力沥青砂岩自生伊利石K-Ar测年与成藏年代[J].石油勘探与开发,2011,38(2):203-210.]
[16]Su Jin,Yang Haijun,Yang Wenjing,et al.The accumulation history of continental oil and the hydrocarbons enrichment mechanism in the Silurian unconformities of the northern Tarim Basin[J].Acta Petrologica Sinica,2012,28(8):2493-2505.[苏劲,杨海军,杨文静,等.塔里木盆地北部志留系顶面不整合中陆源原油的成藏历史与油气富集机制[J].岩石学报,2012,28(8):2493-2505.]
[17]Li Meng,Tang Liangjie,Qi Lixin,et al.Differential tectonic evolution and its controlling on hydrocarbon accumulation in the south slope of Tabei Uplift[J].Natural Gas Geoscience,2015,26(2):218-228.[李萌,汤良杰,漆立新,等.塔北隆起南坡差异构造演化及其对油气成藏的控制[J].天然气地球科学,2015,26(2):218-228.]
[18]Bi Mingwei,Chen Shiyue,Zhou Zhaohua,et al.Densification modes of sandstone reservoir in the 8th member of the Lower Shihezi Formation,Permian,in Su-6 area of Sulige Gasfield,Ordos Basin[J].Geological Review,2015,61(3):599-613.[毕明威,陈世悦,周兆华,等.鄂尔多斯盆地苏里格气田苏6区块二叠系下石盒子组8段砂岩储层致密成因模式[J].地质论评,2015,61(3):599-613.]
[19]Liu Honglin,Zhang Yuzhi,Zhu Minjun,et al.The formation mechanism of secondary quartz of the reservoir[J].Inner Mongolia Petrochemical Industry,2011(4):104-106.[刘洪林,张玉芝,朱敏军,等.储层次生石英形成机理研究[J].内蒙古石油化工,2011(4):104-106.]
[20]Shi Danni,Jin Wei.The origin,migration and precipitation of authigenic quartz in sandstones[J].Lithofacies Palaeogeographic,1999,19(6):65-70.[史丹妮,金巍.砂岩中自生石英的来源、运移与沉淀机制[J].岩相古地理,1999,19(6):65-70.]
[21]Yu Junmin,Zhou Xiaofeng,Liu Li.Genesis and significance of quartz cement in sandstones[J].World Geology,2000,19(1):20-25.[于均民,周晓峰,刘立.砂岩中石英胶结物的成因及其研究意义[J].世界地质,2000,19(1):20-25.]
[22][KG*5/6]Flügel E.Microfacies of Carbonate Rocks[M].Ma Yongsheng,Tian Haiqin,Chen Hongde,et al.Translated.Beijing:Geological Publishing House,2006:614.[Flügel E.碳酸盐岩微相_分析、解释及应用[M].马永生,田海芹,陈洪德,等译.北京:地质出版社,2006:614.]
[23]Yu Hao,Lin Chunming,Zhou Jian,et al.Reservoir characteristics and influencing factors analysis on Early Cretaceous Denglouku and Quantou Formation in the Yaoyingtai area of southern Songliao Basin[J].Acta Sedimentologica Sinica,2012,30(2):240-250.[俞昊,林春明,周健等.松辽盆地南部腰英台地区早白垩世登娄库-泉头组储层特征及影响因素分析[J].沉积学报,2012,30(2):240-250.]
[24]Han Denglin,Li Zhong,Li Weifeng.Heterogeneous features of quartz grain dissolution of Cretaceous sandstone reservoir in the Kuqa Depression and its major controlling factors[J].Acta Geologica Sinica,2011,85(2):256-261.[韩登林,李忠,李维锋.库车坳陷白垩系砂岩储层石英溶蚀非均质性特征及其主控因素[J].地质学报,2011,85(2):256-261.]
[25]Qiu Longwei,Pan Yao.A study on direct dissolution of quartz and its genesis in the Kekeya gas condensate[J].Acta Mineralogica Sinica,2005,25(2):183-190.[邱隆伟,潘耀.柯克亚凝析气田石英的溶解现象及其成因[J].矿物学报,2005,25(2):183-190.]
[26]Xiao Dongsheng,Fu Qiang.The genetic mechanism of authigenic quartz in Lower Shihezi Formation of Hanggin banner,northern Ordos Basin[J].Acta Petrologica et Mineralogica,2011,30(1):113-120.[肖冬生,付强.鄂尔多斯盆地北部杭锦旗区块下石盒子组自生石英形成机制[J].岩石矿物学杂志,2011,30(1):113-120.]
[27]Wang Guanmin.Early diagenesis of the carbonate rock of 1st member of Shahejie Formation in Shanghe area,Huimin Sag[J].Journal of Xi’an Petroleum Institute:Natural Science Edition,2002,17(2):14-17.[王冠民.惠民凹陷沙一段碳酸盐岩的早期成岩作用[J].西安石油学院学报:自然科学版,2002,17(2):14-17.]
[28]Chen Denghui,Gong Enpu,Liang Junhong,et al.Mechanism of the chert formation within the lacustrine carbonates of the Lower Cretaceous Yixian Formation,western Liaoning[J].Acta Geologica Sinica,2010,84(8):1208-1214.[陈登辉,巩恩普,梁俊红,等.辽西下白垩统义县组湖相碳酸盐岩中的燧石成因[J].地质学报,2010,84(8):1208-1214.]
[29]Cheng Zhenbo,Ju Xiaohua,Lan Dongzhao.Study of microfossils in the surface sediments from the CC area of the north-east Pacific Ocean[J].Marine Geology & Quaternary Geology,1998,18(4):43- 51.[程振波,鞠小华,兰东兆.东北太平洋CC区表层沉积物中的微体生物化石研究[J].海洋地质与第四纪地质,1998,18(4):43-51.]
[30]Zhao Guolian.The influence of biogenic procession on the accumulation and precipitation of silica:An example from south of Anhui and west of Zhejiang[J].Acta Sedimentologica Sinica,1999,17(1):30-37.[赵国连.生物作用在二氧化硅聚集沉淀过程中的意义__以皖南浙西的硅岩为例[J].沉积学报,1999,17(1):30-37.]

[1] 沈骋, 赵金洲, 任岚, 范宇. 四川盆地龙马溪组页岩气缝网压裂改造甜点识别新方法[J]. 天然气地球科学, 2019, 30(7): 937-945.
[2] 张晗. 四川盆地龙马溪组页岩储层缝网导流能力优化[J]. 天然气地球科学, 2019, 30(7): 955-962.
[3] 王勇飞, 赵向原, 刘成川. 川东北元坝地区长兴组礁滩相储层裂缝特征及主控因素[J]. 天然气地球科学, 2019, 30(7): 973-981.
[4] 廖凤蓉, 洪峰. 世界巨型气田分布特征及其启示[J]. 天然气地球科学, 2019, 30(6): 860-865.
[5] 张振宇, 张立宽, 罗晓容, 曹斌风, 林会喜, 曾治平, 秦峰, 贺文君, 李超, 雷裕红. 准噶尔盆地中部地区深层西山窑组砂岩成岩作用及其对储层质量评价的启示[J]. 天然气地球科学, 2019, 30(5): 686-700.
[6] 付爽, 庞雷, 许学龙, 曹元婷, 刘振宇, 张顺存, . 准噶尔盆地玛湖凹陷下乌尔禾组储层特征及其控制因素[J]. 天然气地球科学, 2019, 30(4): 468-477.
[7] 陈立超, 王生维, . 煤岩弹性力学性质与煤层破裂压力关系[J]. 天然气地球科学, 2019, 30(4): 503-511.
[8] 谢卫东, 王猛, 代旭光, 王彦迪. 山西河东煤田中—南部煤系页岩气储层微观特征[J]. 天然气地球科学, 2019, 30(4): 512-525.
[9] 姜瑞忠, 张福蕾, 郜益华, 崔永正, 沈泽阳, 原建伟. 三重介质压裂气藏椭圆流非稳态产能模型[J]. 天然气地球科学, 2019, 30(3): 370-378.
[10] 刘树根, 孙玮, 宋金民, 雍自权, 王浩, 赵聪. 四川盆地中三叠统雷口坡组天然气勘探的关键地质问题[J]. 天然气地球科学, 2019, 30(2): 151-167.
[11] 李延丽, 苟迎春, 马新民, 李程程, 王朴, 陈芳芳. 柴达木盆地坪西地区基岩气藏储层特征[J]. 天然气地球科学, 2019, 30(2): 219-227.
[12] 孙秀建, 杨巍, 白亚东, 谢梅, 石正灏. 柴达木盆地基岩油气藏储盖特征及组合方式[J]. 天然气地球科学, 2019, 30(2): 228-236.
[13] 刘虎, 曹涛涛, 戚明辉, 王东强, 邓模, 曹清古, 程斌, 廖泽文. 四川盆地东部华蓥山地区龙潭组页岩气储层特征[J]. 天然气地球科学, 2019, 30(1): 11-26.
[14] 张道锋, 姚泾利, 高星, 席明利, 赵会涛, 闫小雄, 付勋勋. 鄂尔多斯盆地奥陶系马五5亚段白云岩储层形成机理与展布规律[J]. 天然气地球科学, 2019, 30(1): 74-82.
[15] 陈俊飞, 李琦, 朱如凯, 毛治国. 鄂尔多斯盆地陕北地区长101低孔低渗储层孔隙演化及其定量模式[J]. 天然气地球科学, 2019, 30(1): 83-94.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 达江;宋岩;洪峰;赵孟军;傅国友;方世虎;. 中国中西部前陆盆地成藏特征的初步分析[J]. 天然气地球科学, 2006, 17(4): 452 -455 .
[2] 王万春;任军虎;张小军;陶明信;. 黄骅坳陷孔店南区低熟油伴生气地球化学特征与成因[J]. 天然气地球科学, 2006, 17(2): 153 -156 .
[3] 宁 宁;陈孟晋;刘锐娥;孙庆伍;蔺 杰;肖红平;张春林. . 鄂尔多斯盆地东部上古生界石英砂岩储层成岩及孔隙演化[J]. 天然气地球科学, 2007, 18(3): 334 -338 .
[4] 刘春慧;金振奎;朱桂芳;王庆东;张建良. . 准噶尔盆地东部吉木萨尔凹陷二叠系梧桐沟组储层物性特征及控制因素[J]. 天然气地球科学, 2007, 18(3): 375 -379 .
[5] 吴向华,程同锦,邓天龙 . 油气化探分析检测技术现状及发展趋势[J]. 天然气地球科学, 2005, 16(1): 78 -81 .
[6] 李士祥;胡明毅;李霞;. 榆林气田山西组2段砂岩成岩作用及孔隙演化[J]. 天然气地球科学, 2005, 16(2): 200 -205 .
[7] 刘文汇;黄第藩;熊传武;徐永昌;. 成烃理论的发展及国外未熟―低熟油气的分布与研究现状[J]. 天然气地球科学, 1999, 10(1-2): 1 -22 .
[8] 吴时国;袁圣强;. 世界深水油气勘探进展与我国南海深水油气前景[J]. 天然气地球科学, 2005, 16(6): 693 -699 .
[9] 张朝;张廷山;魏祥峰;戴传瑞;王秀林 . 也门X区块下白垩统沉积相分析[J]. 天然气地球科学, 2008, 19(06): 835 -839 .
[10] 陈凤喜 王勇 张吉 杨勇. 鄂尔多斯盆地苏里格气田盒8气藏开发有利区块优选研究[J]. 天然气地球科学, 2009, 20(1): 94 -99 .