天然气地球科学 ›› 2010, Vol. 21 ›› Issue (5): 781–785.doi: 10.11764/j.issn.1672-1926.2010.05.781

• 天然气地质学 • 上一篇    下一篇

流体包裹体分析在划分碳酸盐胶结物形成期次中的应用

孙靖, 金振奎, 薛晶晶   

  1. 1.中国石油新疆油田分公司勘探开发研究院,新疆 克拉玛依 834000;
    2.中国石油大学(北京)资源与信息学院,北京 102249
  • 收稿日期:2009-06-22 修回日期:2010-01-07 出版日期:2010-10-10 发布日期:2010-10-10
  • 通讯作者: 孙靖sun19820804@sina.com. E-mail:sun19820804@sina.com.
  • 作者简介:孙靖(1982-),男,黑龙江黑河人,工程师,主要从事沉积储层研究.
  • 基金资助:

    中国石油天然气集团公司石油中青年创新基金项目(编号:04E7022)资助

Application of Fluidinclusion Analysis in Dividing Formation Stages of Carbonate Cements

SUN Jing, JIN Zhen-Kui, XUE Jing-Jing   

  1. 1.Research Institute of Exploration and Development, Xinjiang Oilfield Company,
    PetroChina, Karamay 834000,China;2.Faculty of Resources and Information, China University of Petroleum (Beijing), Beijing 102249,China.
  • Received:2009-06-22 Revised:2010-01-07 Online:2010-10-10 Published:2010-10-10

摘要:

通过对北京西山露头剖面寒武系和奥陶系岩石裂缝中碳酸盐胶结物中的流体包裹体进行分析,结合地质分析,重点研究了流体包裹体在划分碳酸盐胶结物形成期次中的应用。研究表明,研究区发育的流体包裹体主要为盐水包裹体;包裹体均一温度集中分布在94~98℃和133~145℃这2个区间,相应的盐度区间为4%~8.9%和11.9%~12.5%;碳酸盐胶结物的形成可以分为2期,即Ⅰ期和Ⅱ期,形成深度为1 975~2 075 m和2 950~3 250 m,分别对应于中侏罗世—早白垩世和古近纪,均形成于对流带上部。

关键词: 流体包裹体, 碳酸盐胶结物, 形成期次

Abstract:

The main content in this paper is application of fluid-inclusion analysis in dividing formation stages of carbonate cements that formed in fractures belong to Cambrian and Ordovician rocks of West Hills Peking outcrops. The homogenization temperatures of salt\|water inclusions mainly vary from 94 to 98℃ and 133 to 145℃, corresponding to salinities changing from 4 to 8.9%NaCl and 11.9 to 12.5%NaCl. The carbonate cements that formed from 1975 to 2075m and 2950 to 3250m can be divided into two periods of Ⅰand Ⅱ, corresponding to Middle Jurassic Early Cretaceous and Paleogene, respectively. Both of two periods cements formed in the upper part of convection zone.

Key words: Fluid inclusion, Carbonate cement, Formation stage.

中图分类号: 

  •  

[1]Feng Zengzhao.Lithofacies Paleogeography of Early Paleozonic of North China Platform[M].Beijing:Geological Publishing House,1999:3-25.[冯增昭.华北地台早古生代岩相古地理[M].北京:地质出版社,1999:3-25.]
[2]Jin Zhenkui,Zhang Xiangxiang,Zou Yuanrong,et al.Precipitation sequence of carbonate cement of the Ordovician in Qianmiqiao area,Huanghua depression[J].Journal of Palaeogeography,2003,5(4):426-438.[金振奎,张响响,邹元荣,等.黄骅坳陷千米桥地区奥陶系碳酸盐胶结物形成序次[J].古地理学报,2003,5(4):426-438.]
[3]Chen Lihua,Wang Jiahua.Hydrocarbon Reservoir Research Technology[M].Beijing:Petroleum Industry Press,2000:176-197.[陈丽华,王家华.油气储层研究技术[M].北京:石油工业出版社,2000:176-197.]
[4]Chi Guoxiang,Zhou Yiming,Lu Huanzhang.An overview on current fluid-inclusion research and application[J].Acta Petrologica Sinica,2003,19(2):201-212.[池国祥,周义明,卢焕章.当前流体包裹体研究和应用概况(英文)[J].岩石学报,2003,19(2):201-212.] 
[5]Feng Zihui,Ren Yanguang,Wang Cheng,et al.Study on inclusion of deep buried igneous reservoir and forming period of gas pool in Songliao basin[J].Natural Gas Geoscience,2003,14(6):436-442.[冯子辉,任延广,王成,等.松辽盆地深层火山岩储层包裹体及天然气成藏期研究[J].天然气地球科学,2003,14(6):436-442.]
[6]Li Xianqing,Hu Guoyi,Li Jian,et al.The characteristics of fluid inclusion and its pool-forming significance of natural gas from Ordovician carbonate reserviors in central Ordos basin[J].Natural Gas Geoscience,2004,15(2):120-124.[李贤庆,胡国艺,李剑,等.鄂尔多斯盆地中部奥陶系碳酸盐岩储层流体包裹体特征及对天然气成藏的意义[J].天然气地球科学,2004,15(2):120-124.]
[7]Xu Hao,Tang Dazhen,Wei Guoqi,et al.Study on the hydrocarbon charge history in the 2nd member of Xujiahe Formation of west Sichuan by evidence from fluid in clusions[J].Natural Gas Geoscience,2005,16(5):571-574.[许浩,汤达祯,魏国齐,等.川西地区须二段油气充注历史的流体包裹体分析[J].天然气地球科学,2005,16(5):571-574.]
[8]Mi Jingkui,Dai Jinxing,Zhang Shuichang.Some problem existed in research of inclusion occurring in oil and gas bearing basin[J].Natural Gas Geoscience,2005,16(5):602-605.[米敬奎,戴金星,张水昌.含油气盆地包裹体研究中存在的问题[J].天然气地球科学,2005,16(5):602-605.]
[9]Liao Shimeng,Wang Qiang,Xu Zhiming,et al.The questions in application of inclusion composition analytical technique[J].Natural Gas Geoscience,2006,17(2):170-172.[廖仕孟,王强,徐志明,等.流体包裹体分子组成分析技术应用中存在的问题[J].天然气地球科学,2006,17(2):170-172.]
[10]Wang Tieguan,Jin Zhenkui,Wang Darui,et al.Applications of Inorganic Geochemistry in Petroleum Geology[M].Beijing:Petroleum Industry Press,1999:38-49.[王铁冠,金振奎,王大锐,等.无机地球化学在石油地质学中的应用[M].北京:石油工业出版社,1999:38-49.]
[11]Liu Xin,Yang Chuanzhong.Principal research methods on mineral fluid inclusions of carbonate rock and their applications[J].Experimental Petroleum Geology,1991,13(4):399-406.[刘鑫,杨传忠.碳酸盐岩矿物流体包裹体的主要研究方法及其应用[J].石油实验地质,1991,13(4):399-406.]
[12]Hall D L.Freezing point depression of NaCl-KCl-H2O solution[J].Economic Geology,1988,8(3):197-202.

[1] 孙可欣,李贤庆,魏强,梁万乐,李剑,张光武. 利用流体历史分析技术研究库车坳陷大北气田油气充注史[J]. 天然气地球科学, 2018, 29(9): 1289-1300.
[2] 杨超,贺永红,马芳侠,雷裕红,陈义国. 鄂尔多斯盆地南部三叠系延长组有机流体活动期次划分[J]. 天然气地球科学, 2018, 29(5): 655-664.
[3] 陈兰朴,李国蓉,吴章志,朱亚林,符浩,高鱼伟,王雨辰,王冬娅,何赛,胡静. 塔里木盆地塔河油田东南斜坡海西晚期奥陶系热液作用[J]. 天然气地球科学, 2017, 28(3): 410-419.
[4] 郭佳佳,孙国强,龙国徽,管斌,康健,夏维民,陈波,史基安. 柴达木盆地北缘冷湖五号构造下侏罗统沉积—成岩环境分析[J]. 天然气地球科学, 2017, 28(12): 1839-1845.
[5] 王琳,赵孟军,孟庆洋,王鹏,王科,袁海莉,申磊军,雷刚. 柴达木盆地英西地区中深层油气成藏过程分析[J]. 天然气地球科学, 2017, 28(12): 1846-1854.
[6] 孙先如,贾超,李振生,李建勋,曹高社. 南华北盆地寒武系底部马店组气源岩演化的流体包裹体分析[J]. 天然气地球科学, 2017, 28(11): 1625-1636.
[7] 王萍,潘文蕾,陈迎宾,吴小奇,王保华. 川西坳陷中段须四段天然气成藏期次研究[J]. 天然气地球科学, 2016, 27(8): 1419-1426.
[8] 吴海,赵孟军,白东来,周延钊,周彦臣. 库车前陆盆地吐北2构造油气充注过程分析[J]. 天然气地球科学, 2016, 27(4): 600-608.
[9] 孙国强,陈波,郑永仙,谢梅,夏维民,史基安. 柴北缘冷湖五号构造中新统成岩作用及沉积环境[J]. 天然气地球科学, 2015, 26(4): 679-688.
[10] 赵洪,罗晓容,张立宽,林会喜,许涛,胡才志,杨彬,雷裕红,路永扬. 准噶尔盆地中部1区块三工河组流体包裹体特征及对油气多期充注—调整过程的指示[J]. 天然气地球科学, 2015, 26(3): 466-476.
[11] 孟庆洋,桂丽黎,陈琰,袁莉,杨帆,隋立伟,白东来. 柴达木盆地西南地区典型油田油气充注期研究[J]. 天然气地球科学, 2015, 26(2): 252-260.
[12] 曹青,高俊梅,范立勇,庞长旭,余金柱. 鄂尔多斯盆地西南部上古生界流体包裹体特征及其意义[J]. 天然气地球科学, 2015, 26(12): 2245-2253.
[13] 刘建良,姜振学,刘可禹,桂丽黎,李峰,邢金艳. 库车前陆盆地牙哈构造带油气成藏过程研究[J]. 天然气地球科学, 2015, 26(1): 43-53.
[14] 陈哲龙,柳广弟,卢学军,黄志龙,丁修建. 应用流体包裹体研究储层油气充注特征——以二连盆地为例[J]. 天然气地球科学, 2015, 26(1): 60-70.
[15] 孙国强,王海峰,邹开真,王文卓,周刚,马进业,陈章群. 柴北缘九龙山地区侏罗系砂岩中碳酸盐胶结物特征及意义[J]. 天然气地球科学, 2014, 25(9): 1358-1365.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!