Advanced Search

LIU De liang, TAN Ying, SUN Xian ru, LI Zheng sheng, FANG Guo qing, TAO Shi zheng. Characteristics of Erathem Fluid Inclusions and Their Relationship with Oil-gas Evolution in Ordos Basin[J]. Acta Sedimentologica Sinica, 2002, 20(4): 695-704.
Citation: LIU De liang, TAN Ying, SUN Xian ru, LI Zheng sheng, FANG Guo qing, TAO Shi zheng. Characteristics of Erathem Fluid Inclusions and Their Relationship with Oil-gas Evolution in Ordos Basin[J]. Acta Sedimentologica Sinica, 2002, 20(4): 695-704.

Characteristics of Erathem Fluid Inclusions and Their Relationship with Oil-gas Evolution in Ordos Basin

  • Received Date: 2001-07-11
  • Rev Recd Date: 2001-10-29
  • On the base of research on diagenesis of Ordovivian carbonati te and quartzose sandstone in Ordos basin, preliminary S tudy on inclusio ns in these rocks have been done.There are three sections of homgogenization temperature of inclusio ns in Ordovician carbonate rock :60 ℃~ 100 ℃, 100 ℃~ 160 ℃, 160 ℃~ 220 ℃;and there are three sections of homogenization temperature of inclusions in Permocarboniferous quartzose;90 ℃~ 110 ℃, 120 ℃~140 ℃, 160 ℃~ 220℃.Making use of temperature data of inclusions combined w ith the recently research result of vitrinite reflectivity and apatite fission track, the paper discussed the application of fluid inclusions to formation and evolution of oil-gas reservoirs in Ordos basin.
  • [1] 刘德良,谈迎,孙先如,戴金星等. 鄂尔多斯流体包裹体与天然气生成运移的研究[R].2000[Liu Deliag, Tan Ying, Sun Xianru, et al. Research of fluid inclusion for mation and transport of natural gas in Ordos Basin[R]. 2000.30~87]
    [2] 陶士振,刘德良,杨晓勇等. 塔里木盆地叶城凹陷成岩包裹体及其油气意义[J].石油学报,1998,19(3):38~45[Tao Shizheng, Liu Deliang, Yang Xiaoyong, et al, Yecheng depression diagenesis inclusions and implication to oil and gas in Tarim Basin[J]. Acta Petrolei Sinica, 1998,19(3):38~45]
    [3] 杨晓勇,刘德良,陶士振. 中国东部典型地幔岩中包裹体成分及意义[J]. 石油学报,1999,20(1):19~23[Yang Xiaoyong, Liu Deliang, Tao Shizheng. Compositions and implications of inclusions in the typical mantle rocks form east China[J]. Acta Petrolei Sinica, 1999, 20(1):19~23]
    [4] 杨晓勇,郑永飞,刘德良,等.中国东部橄榄岩包裹体和榴辉岩中CO2流体包裹体的碳同位素组成[J].岩石学报,2000,16(4):473~481[Yang Xiaoyong,Zheng Yongfei,Liu Deliang, et al. Carbon isotope composition of carbon dioxde in fluid inclusions from peridotite xenoltite xenoliths and eclogites in East China[J]. Acta Petrologica Sinica, 2000, 16(4): 473~481]
    [5] 刘德良,宋岩,薛爱民等.四川盆地构造与天然气聚集区带[M]. 北京:石油出版社,2000[liu Deliang,Song Yan, Xue Aimin, et al. Structure of Sichuan basin and enrichment belt of natural gas[M]. Beijing: Petroleum Publising House, 2000]
    [6] 孙先如,李院生,董树文等.大别山榴辉岩的包裹体研究[J].矿物学报,1995,15(3):352~359[Sun Xianru, Li Yuangsheng, Dong Shuwen, et al. Research on inclusions in eclogite of Dabie Mount[J]. Acta Mineralogica Sinica, 1995,15(3):352~359]
    [7] 张永生,张传录,康祺发.鄂尔多斯盆地奥陶系马家沟群块状白云岩包裹体研究[J].岩石矿物学杂志,1997,16(3):213~219[Zhang Yongsheng,Zhang Chunlu,Kang Qifa. Research on inclusions in massive dolostones in the Majiagou group of Ordovician,Ordos Basin[J]. Acta Petrologica et Mineralogica, 1997,16(3):213~219]
    [8] 张永生. 鄂尔多斯地区奥陶系马家沟群中部块状白云岩的深埋藏白云石化机制[J].沉积学报,2000,18(3):424~430[Zhang Yongsheng. Mechanism of deep burial dolomitization of massive dolodtones in the middle Majiagou group of the Ordovician, Ordos basin[J]. Acta Sedimentologica Sinica, 2000, 18(3):424~430]
    [9] 郑葆英,叶俭,祝总祺,宋国初. 鄂尔多斯盆地奥陶系马家沟组气液包裹体研究[J].西安工程学院学报,1999,21(3):13~16[Zheng Baoying, Ye Jian, Zhu Zongqi, et al. Study of the fluid inclusions from the Majiangou Formation of Ordovician, Ordos Basin[J]. Journal of Xi'an engineering university, 1999,21(3):13~16]
    [10] 谢奕汉,范宏瑞,王英兰. 流体包裹体与盆地油气的生成和演化[J].地质科技情报增刊,1998, 17:100~104[Xie Yihan, Fan Hongrui, Wang Yinglan. Fluid inclusions and their relation to the formation and evolution of oil-gas in a basin[J]. Geological Science and Techology Information, 1988,17:100~104]
    [11] 赵孟为. 鄂尔多斯盆地油气形成与运移时间和运移方向的确定与勘探方向[J].石油实验地质,1996,18(4):341~347[Zhao Mengwei. Timing of hydrocarbon generation and transport and determination of transport direction as well as exploration direction in the Ordos Basin[J]. Experimental Petroleum Geology, 1996,18(4):341~347]
    [12] Waples D W. Time and temperature in petroleμm fomation:application of Lopatin's method to petroleμm exploration[J]. AAPG Bull, 1980,64:916~926
    [13] Tissot B P, Welte D M. Petroleum formation and occurrence[M]. Berlin:Spinger-Verlag, 1984.699
    [14] Quigley T M, et al. Kinetic theory of petroleum generation[A]. In: Doligez B ed. Migration of hydrocarbons in sedimentary basins[C].Paris: Editions Technip. 1987,649~666
    [15] Quigley T M and Mackenzie A S. The temperatures of oil and gas formation in the sub-surface [J]. Nature, 1988,333:549~552
    [16] 傅家谟,史继扬.石油演化理论与实践(1)-石油演化机理与石油演化阶段[J].地球化学,1975, 2: 87~107[Fu Jiamo, Shi Jiyang.Theory and practice of petroleum evolution(1)-evolution mechanism and evolution stage of petroleum[J].Geochemistry,1975,2:87~107]
    [17] 任战利,赵重远,张军,于忠平. 鄂尔多斯盆地古地温研究[J].沉积学报,1994,12(1):56~65[Ren Zhanli, Zhao Chongyuan,Zhang Jun, et al. Research on paleo-temperature of Ordos basin[J]. Acta Sedimentologica Sinica, 1994,12(1):56~65]
    [18] 赵孟为,Hans Ahrendt, Klaas Wemmer. K-Ar测年法在确定沉积岩成岩时代中的应用-以鄂尔多斯盆地为例[J].沉积学报,1996,14(3):11~21[Zhao Mengwei, Hans Ahredt, Klass Wemmer. Application of K-Ar dating to the diagenesis time of sedimentary rock-Taking Ordos basin for example[J]. Acta Sedientologica Sinica, 1996,14(3):11~21]
    [19] 刘宝王君.沉积岩石学[M].北京:地质出版社,1980[Liu Baojun. Sedimentary petrology[M].Beijing:Geological Publishing House,1980]
    [20] Barker C E and Pawlewicz M T. The Correlation of Vitrinite reflectance with maximum temperature in hnumic organic matter paleaogeothermics Lecture Note in Earth Sciences[M]. Berlin: Springer-verlag,1986.5 79~93
    [21] 任战利. 鄂尔多盆地演化史与油气关系[J].石油学报,1996,17(1):17~23[Ren Zhanli. Relationship of evolution with oil-gas in Ordos Basin[J]. Acat, Petrolei Sinica, 1996,17(1):17~23]
    [22] Xiao-Yong Yang, Yong-Fei Zheng, De-Liang Liu, et al. Chemical and carbon isotope composition of fluid inclusions in peridotite xenoliths and eclogites from eastern China: Geodynamic implications[J]. Physics and Chemistry of the Earth, 2001, 26(9~10):705~718
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(247) PDF downloads(18) Cited by()

Proportional views
Related
Publishing history
  • Received:  2001-07-11
  • Revised:  2001-10-29

Characteristics of Erathem Fluid Inclusions and Their Relationship with Oil-gas Evolution in Ordos Basin

Abstract: On the base of research on diagenesis of Ordovivian carbonati te and quartzose sandstone in Ordos basin, preliminary S tudy on inclusio ns in these rocks have been done.There are three sections of homgogenization temperature of inclusio ns in Ordovician carbonate rock :60 ℃~ 100 ℃, 100 ℃~ 160 ℃, 160 ℃~ 220 ℃;and there are three sections of homogenization temperature of inclusions in Permocarboniferous quartzose;90 ℃~ 110 ℃, 120 ℃~140 ℃, 160 ℃~ 220℃.Making use of temperature data of inclusions combined w ith the recently research result of vitrinite reflectivity and apatite fission track, the paper discussed the application of fluid inclusions to formation and evolution of oil-gas reservoirs in Ordos basin.

LIU De liang, TAN Ying, SUN Xian ru, LI Zheng sheng, FANG Guo qing, TAO Shi zheng. Characteristics of Erathem Fluid Inclusions and Their Relationship with Oil-gas Evolution in Ordos Basin[J]. Acta Sedimentologica Sinica, 2002, 20(4): 695-704.
Citation: LIU De liang, TAN Ying, SUN Xian ru, LI Zheng sheng, FANG Guo qing, TAO Shi zheng. Characteristics of Erathem Fluid Inclusions and Their Relationship with Oil-gas Evolution in Ordos Basin[J]. Acta Sedimentologica Sinica, 2002, 20(4): 695-704.
Reference (22)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return