吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (6): 1649-1657.doi: 10.13278/j.cnki.jjuese.20180211

• 地质与资源 • 上一篇    下一篇

松辽盆地南部地区营城组典型火山机构地质特征

迟唤昭1, 董福湘1, 薛晓刚1, 刘财2, 司考3   

  1. 1. 长春工程学院勘查与测绘工程学院, 长春 130021;
    2. 吉林大学地球探测科学与技术学院, 长春 130026;
    3. 吉林大学校友联络和教育基金管理处, 长春 130012
  • 收稿日期:2018-08-10 发布日期:2019-11-30
  • 作者简介:迟唤昭(1985-),男,博士研究生,讲师,主要从事火山岩地质-地球物理勘探方向研究,E-mail:chihz680@sina.com
  • 基金资助:
    吉林省科技发展计划项目（20180101310JC）；吉林省教育厅科学技术项目（JJKH20180990KJ）；长春工程学院校基金项目（320160015）

Geological Characteristics of Typical Volcanic Edifices of Yingcheng Formation in Southern Songliao Basin

Chi Huanzhao1, Dong Fuxiang1, Xue Xiaogang1, Liu Cai2, Si Kao3   

  1. 1. School of Prospecting & Surveying Engineering, Changchun Institute of Technology, Changchun 130021, China;
    2. College of GeoExploration Science and Technology, Jilin University, Changchun 130026, China;
    3. Fund Management Office, Jilin University, Changchun 130012, China
  • Received:2018-08-10 Published:2019-11-30
  • Supported by:
    Supported by the Science and Technology Department Project of Jilin Province (20180101310JC), the Education Department Project of Jilin Province (JJKH20180990KJ) and Changchun Institute of Technology Project (320160015)

PDF (PC)

365

摘要： 在松辽盆地地质背景研究的基础上，根据盆地南部地区营城组火山岩地质特征对火山机构进行分类，描述其地质特征，并讨论其储层特征。将研究区火山机构分成3类9种，即熔岩类火山机构、碎屑岩类火山机构和复合火山机构3类；熔岩类火山机构包括粗面质熔岩火山机构、玄武质熔岩火山机构、安山质熔岩火山机构、英安质熔岩火山机构和流纹质熔岩火山机构，碎屑岩类火山机构包括玄武质碎屑岩火山机构、安山质碎屑岩火山机构和流纹质碎屑岩火山机构，以及复合火山机构共计9种。并统计了不同类型流纹质火山机构储层的储集空间类型及孔隙度，结果表明：流纹质复合火山机构储集空间类型复杂，储层溶蚀孔缝十分发育，储层物性最好；流纹质碎屑岩火山机构储层溶蚀孔缝较为发育，储层物性中等；流纹质熔岩火山机构储集空间类型单一，储层物性最差。将长岭断陷火山机构内部储层分为高孔-高渗型、中孔-中渗型和低孔-低渗型3类，且有利储层受岩性影响较小，受岩相影响较大。

关键词: 松辽盆地, 营城组, 火山机构, 储层物性, 流纹质, 长岭断陷

Abstract: This study aims to construct the volcanic edifices,and discuss the characteristics of the different volcanic edifices and the reservoir of Yingcheng Formation in the southern area of Songliao Basin. The volcanic edifices of the study area are divided into 3 kinds and 9 types (trachytic lava, basaltic lava, andesitic lava, dacitic lava, rhyolitic lava, basaltic clastic rock, andesitic clastic rock, rhyolitic clastic rock,and composite volcanic edifices). In addition, the statistics of different reservoir types and porosity suggest that the rhyolitic composite volcanic edifices have the best reservoir characteristics, and the solution pores are important pore type; rhyolitic clastic volcanic edifices have the worse and the worst reservoir characteristics belong to the rhyolitic lava. The reservoir in Changling fault depression is divided into three types:high porosity-high permeability reservoir, middle porosity-middle permeability reservoir, and low porosity-low permeability reservoir. The favorable reservoir is mainly affected by lithofacies rather than lithology.

Key words: Songliao basin, Yingcheng Formation, volcanic edifices, reservoir characteristics, rhyolitic, Changling fault depression

中图分类号: 

  • P317.2
[1] 张立伟,师永民,李江海.徐家围子营城组一段火山岩旋回测井响应特征[J].北京大学学报(自然科学版),2009, 45(3):481-487. Zhang Liwei, Shi Yongmin, Li Jianghai. Logging Response to the Volcanic Cycles of the First Member of Yingcheng Formation in Xujiaweizi Fault Depression[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2009,45(3):481-487.
[2] 黄玉龙,王璞珺,门广田,等.松辽盆地南部营城组火山岩旋回、期次划分方法:以盆缘剖面和盆内钻井为例[J].吉林大学学报(地球科学版),2007, 37(6):1183-1192. Huang Yulong, Wang Pujun, Men Guangtian, et al. Division of Volcanic Cycles and Stages of the Yingcheng Formation of the Songliao Basin:Take the Cross Sections at the Margin and the Boring Holes as Examples[J]. Journal of Jilin University(Earth Science Edition), 2007, 37(6):1183-1192.
[3] 胡佳, 王立武, 张双杰, 等. 盆地内部火山机构的地质模式建立方法及其应用:以松辽盆地南部地区营城组火山岩为例[J]. 西安石油大学学报(自然科学版), 2018, 33(6):18-26. Hu Jia, Wang Liwu, Zhang Shuangjie, et al.Establishment of Geological Modes of Volcanic Structures Within Basins and Its Application:A Case Study on the Volcanic Rocks of Yingcheng Formation in Southern Songliao Basin[J]. Journal of Xi'an Shiyou University(Natural Science Edition), 2018,33(6):18-26.
[4] 丁林,周勇,张进江,等.藏北鱼鳞山新生代火山岩及风化壳符合堆积物的组成和时代[J].科学通报,2000, 45(14):1475-1481. Ding Lin, Zhou Yong, Zhang Jinjiang, et al. Constitution and Age of the Cenozoic Volcanics and Compounded Accumulations of Weathering Crust in Mount Yulin, Northern Tibet[J]. Chinese Scinece Bulletin, 2000,45(14):1475-1481.
[5] Thouret J C. Volcanic Geomorphology:An Overview[J]. Earth-Science Reviews, 1999, 47:95-111.
[6] Thordarson T, Larsen G. Volcanism in Iceland in Historical Time:Volcano Types, Eruption Styles and Eruptive History[J]. Journal of Geodynamics, 2007,43:118-152.
[7] 黄玉龙,王璞珺,冯志强,等.松辽盆地改造残留古火山机构与现代火山机构的类比分析[J].吉林大学学报(地球科学版), 2007, 37(1):65-72. Huang Yulong, Wang Pujun, Feng Zhiqiang, et al. Analogy of Volcanic Edifices Between Modern Volcanoes and Ancient Remnant Volcanoes in Songliao Basin[J]. Journal of Jilin University(Earth Science Edition), 2007, 37(1):65-72.
[8] 谭佳奕,王淑芳,吴润江,等.新疆东准噶尔石炭纪火山机构类型与时限[J].岩石学报, 2010, 26(2):440-448. Tan Jiayi, Wang Shufang, Wu Runjiang, et al. Types and Time of Carboniferous Volcanic Edifices in Eastern Junggar, Xinjiang[J]. Acta Petrologica Sinica, 2010, 26(2):440-448.
[9] 衣健,单玄龙,唐华风,等.盆地埋藏火山机构的地质-地球物理二维精细解剖:以松南腰英台地区营城组一段为例[J].地球物理学报, 2011, 54(2):588-596. Yi Jian, Shan Xuanlong, Tang Huafeng, et al. The Geological-Geophysical Two-Dimensional Dissection of Basin Buried Volcanic Edifices:Take the First Member of Yingcheng Formation in Yaoyingtai Regional of Southern Songliao Basin as Example[J]. Chinese Journal of Geophysics, 2011, 54(2):588-596.
[10] 王亚楠, 李占东. Y断陷营城组火山机构特征及演化[J]. 地球物理学进展, 2017, 32(4):1673-1678. Wang Yanan, Li Zhandong.Volcanic Apparatus Feature and Evolution of Y Fault Depression in Yingcheng Group[J]. Progress in Geophysics, 2017, 32(4):1673-1678.
[11] 严清高, 江小均, 吴鹏, 等. 滇中姚安老街子板内富碱火山岩锆石SHRIMP U-Pb年代学及山机构划分[J]. 地质学报, 2017, 91(8):1743-1759. Yan Qinggao, Jiang Xiaojun, Wu Peng,et al. Zircon SHRIMP U-Pb Geochronology and Volcanic Edifice Division of Laojiezi Intraplate Alkali-Rich Volcanic Rocks in Yao'an, Central Yunnan Province[J]. Acta Geologica Sinica, 2017, 91(8):1743-1759.
[12] 杨爱雪, 孙德有, 苟军, 等. 大兴安岭北部上护林盆地恩和大岭火山机构特征与时代[J]. 世界地质, 2016, 35(3):687-696. Yang Aixue, Sun Deyou, Gou Jun,et al. Characteristics and Time of Enhedaling Volcanic Edifice from Shanghulin Basin in Northern Great Xing'an Range[J]. Global Geology, 2016, 35(3):687-696.
[13] 任利军, 单玄龙, 王璞珺, 等. 松辽盆地营城组古火山机构的剖析:以东南隆起区三台珍珠岩山为例[J]. 吉林大学学报(地球科学版), 2007, 37(6):1159-1165. Ren Lijun, Shan Xuanlong, Wang Pujun, et al. Analysis of Ancient Volcanic Edifices of Yingcheng Formation in Songliao Basin:Examples from the Mountain of Perlite in Santai, Southeast Uplift[J]. Journal of Jilin University(Earth Science Edition), 2007, 37(6):1159-1165.
[14] Walker G P L. Explosive Volcanic Eruptions:A New Classification Scheme[J]. International Journal of Earth Sciences, 1973, 62(2):431-446.
[15] 陆建林,王果寿,蔡进功,等.长岭断陷火山岩气藏勘探潜力[J].天然气工业,2007,27(8):13-15. Lu Jianlin, Wang Guoshou, Cai Jingong, et al. An Analysis of Exploration Potential of Volcanic Gas Pools in Changling Fault Depression[J]. Natural Gas Industry, 2007,27(8):13-15.
[16] 单玄龙,高璇,徐汉梁. 松辽盆地安达地区营城组中基性火山岩成藏主控因素[J]. 吉林大学学报(地球科学版), 2012, 42(5):1348-1357. Shan Xuanlong, Gao Xuan, Xu Hanliang. The Main Factors of Intermediate and Mafic Volcanic Gas Reservoir Forming of Yingcheng Formation in Anda Area of Songliao Basin[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(5):1348-1357.
[17] Shan Xuanlong, Li Jiyan, Chen Shumin, et al. Subaquatic Volcanic in Continental Facies and Their Influence on High Quality Source Rocks Shown by the Volcanic Rocks of a Faulted Depression in Northeast China[J]. Science China Earth Sciences,2013, 56(11):1926-1933.
[18] 任宪军,单玄龙,衣健. 松辽盆地长岭断陷营城组火山熔岩流单元储层特征及量化表征[J]. 中国石油大学学报(自然科学版), 2017, 41(5):30-40. Ren Xianjun, Shan Xuanlong, Yi Jian. Characteristics and Quantitative Evaluation of Reservoir in Lava Flow Units in the Early Cretaceous Yingcheng Formation in Changling Depression of Songliao Basin[J]. Journal of China University of Petroleum(Edition of Natural Science), 2017, 41(5):30-40.
[19] 蒋飞,程日辉,许中杰,等. 火山岩冷却单元及其天然气成藏意义:以松辽盆地王府断陷为例[J].天然气地球科学, 2015,26(12):2281-2291. Jiang Fei, Cheng Rihui, Xu Zhongjie, et al. Volcanic Cooling Unit and Its Significance on Natural Gas Accumulation:A Case Study from Wangfu Fault Depression in Songliao Basin[J]. Natural Gas Geoscience, 2015,26(12):2281-2291.
[20] 邹才能,赵文智,贾承造,等.中国沉积盆地火山岩油气藏形成与分布[J]. 石油勘探与开发,2008, 35(3):257-271. Zou Caineng, Zhao Wenzhi, Jia Chengzao, et al. Formation and Distribution of Volcanic Hydrocarbon Reservoirs in Sedimentary Basins of China[J]. Petroleum Exploration and Development, 2008,35(3):257-271.
[21] 王璞珺,吴河勇,庞颜明,等.松辽盆地火山岩相:相序、相模式与储层物性的关系[J].吉林大学学报(地球科学版),2006,36(5):805-812. Wang Pujun, Wu Heyong, Pang Yanming, et al. Volcanic Facies of the Songliao Basin:Sequence, Model and the Quantitative Relationship with Pporosity & Permeability of the Volcanic Reservoir[J]. Journal of Jilin University (Earth Science Edition), 2006, 36(5):805-812.
[22] 姜雪,邹华耀,饶勇,等.松辽盆地南部长岭断陷火山岩岩性岩相特征及其对储层的控制作用[J].科技导报, 2009,27(23):32-40. Jiang Xue, Zou Huayao, Rao Yong,et al. Lithologic and Lithofacies Characteristics of Volcanic Rock and Their Controlling Effects on Reservoirs of Changling Fault Depression in the South of Songliao Basin[J]. Science & Technology Review, 2009,27(23):32-40.
[23] 魏星,孙寅森. 南堡凹陷火山岩岩相对储层的控制作用[J]. 特种油气藏, 2009,24(1):27-31. Wei Xing, Sun Yinsen. Control of Lithofacies of Volcanic Rocks over Reservoirs in the Nanpu Sag[J]. Special Oil & Gas, 2009,24(1):27-31.
[24] 卢志远, 张晓黎, 蒋庆平,等. 准噶尔盆地东部石炭系火山岩储层特征[J].科学技术与工程, 2017,17(35):217-221. Lu Zhiyuan, Zhang Xiaoli, Jiang Qingping, et al. Characteristics of the Carboniferous Volcanic Reservoirs in the Eastern Junggar Basin[J]. Science Technology and Engineering, 2017,17(35):217-221.
[1] 陈思芮, 曲希玉, 王冠民, 王清斌, 曹英权. 渤中凹陷CFD18-2油田高岭石胶结作用及其对储层物性的影响[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1235-1246.
[2] 周翔. 松辽盆地北部营城组火山岩地球化学特征及地质意义[J]. 吉林大学学报(地球科学版), 2019, 49(4): 1001-1014.
[3] 王坤, 曾昭发, 张良怀, 李静, 鹿琪, 张建民. 伊通盆地横头山火山机构综合地球物理探测[J]. 吉林大学学报(地球科学版), 2018, 48(5): 1522-1531.
[4] 马国庆, 孟庆发, 黄大年. 基于重力异常的松辽盆地构造特征识别[J]. 吉林大学学报(地球科学版), 2018, 48(2): 507-516.
[5] 蔡来星, 卢双舫, 肖国林, 王蛟, 吴志强, 郭兴伟, 侯方辉. 论优质源储耦合关系的控藏作用:对比松南致密油与松北致密气成藏条件[J]. 吉林大学学报(地球科学版), 2018, 48(1): 15-28.
[6] 唐华风, 赵鹏九, 高有峰, 王璞珺, 齐雨宁. 盆地火山地层时空属性和岩石地层单位[J]. 吉林大学学报(地球科学版), 2017, 47(4): 949-973.
[7] 鲍新华, 张宇, 李野, 吴永东, 马丹, 周广慧. 松辽盆地增强型地热系统开发选区评价[J]. 吉林大学学报(地球科学版), 2017, 47(2): 564-572.
[8] 高翔, 刘志宏, 聂志阳, 姚勇, 贾卧, 王超, 宋健. 松辽盆地大庆长垣形成时间的厘定及其地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(1): 74-83.
[9] 林承焰, 曹铮, 任丽华, 张昌盛, 范瑞峰, 王叶, 邢新亚, 马晓兰. 松辽盆地南部大情字井向斜区葡萄花油层石油富集规律及成藏模式[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1598-1610.
[10] 邱隆伟, 师政, 付大巍, 潘泽浩, 杨生超, 曲长胜. 临南洼陷沙三段孔隙度控制因素分析与定量模型[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1321-1331.
[11] 刘财, 杨宝俊, 冯晅, 单玄龙, 田有, 刘洋, 鹿琪, 刘才华, 杨冬, 王世煜. 论油气资源的多元勘探[J]. 吉林大学学报(地球科学版), 2016, 46(4): 1208-1220.
[12] 康健, 韦庆海, 周琳, 高研, 张永刚, 高峰. 利用地震台阵观测资料研究大庆地区深部构造[J]. 吉林大学学报(地球科学版), 2016, 46(3): 900-910.
[13] 温志良, 姜福平, 钟长林, 姜雪飞, 王果谦, 齐岩. 松辽盆地东南隆起超大型油页岩矿床特征及成因[J]. 吉林大学学报(地球科学版), 2016, 46(3): 681-691.
[14] 修立君, 邵明礼, 唐华风, 董常春, 高有峰. 松辽盆地白垩系营城组火山岩孔缝单元类型和特征[J]. 吉林大学学报(地球科学版), 2016, 46(1): 11-22.
[15] 那金, 许天福, 魏铭聪, 冯波, 鲍新华, 姜雪. 增强地热系统热储层-盐水-CO2相互作用[J]. 吉林大学学报(地球科学版), 2015, 45(5): 1493-1501.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发