Zhang Lin, Wei Guoqi, Wu Shixiang, Wang Zecheng, Xiao Xianming, Zhang Peijun, Sheng Juehong. DISTRIBUTION CHARACTERS AND HYDROCARBON-GENERATING POTENTIAL OF BITUMEN OF SINIAN-LOWER PALEOZOIC IN SICHUAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2005, 27(3): 276-280. doi: 10.11781/sysydz200503276
Citation: Zhang Lin, Wei Guoqi, Wu Shixiang, Wang Zecheng, Xiao Xianming, Zhang Peijun, Sheng Juehong. DISTRIBUTION CHARACTERS AND HYDROCARBON-GENERATING POTENTIAL OF BITUMEN OF SINIAN-LOWER PALEOZOIC IN SICHUAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2005, 27(3): 276-280. doi: 10.11781/sysydz200503276

DISTRIBUTION CHARACTERS AND HYDROCARBON-GENERATING POTENTIAL OF BITUMEN OF SINIAN-LOWER PALEOZOIC IN SICHUAN BASIN

doi: 10.11781/sysydz200503276
  • Received Date: 2004-02-15
  • Rev Recd Date: 2005-04-22
  • Publish Date: 2005-05-25
  • This paper systematically studies the sort,origin,distribution,capability of hydrocarbon-generating,and main gas-generating times of the bitumen of Sinian-Lower Paleozoic in Sichuan basin.Based on the whole rock polished surfaces configuration and optical characteristic,the bitumen is sorted five types.It has two origin kinds,one is original-in the bed bitumen which mostly distributed in the dark mudstone,fine sandy mudstone,the other is secondary-reservoir bitumen which mostly distributed in the carbonate reservoir rock.Bitumen distributed widely in Dengying formation,its content is higher,from depression (where account for 0.41%)to slope (0.93%~1.13%)and to uplift (2.4%~5.41%),which means higher content in Leshang-Longnusi Paleo-uplift.The Bitumen has high content in weathering zone and become less far from the zone.The Bitumen of Dengying formation of Sinian forms in middle Jurassic,its the main gas-generating time is early Cretaceous which is later than koregen.The Bitumen has strong capability of hydrocarbon-generating which can accumulate to middle gas field.

     

  • loading
  • [1]
    刘德汉,史继扬.高演化碳酸盐岩非常规评价方法探讨[J].石油勘探与开发,1994,21(3):113~115
    [2]
    刘德汉,周中毅,贾蓉芬等.碳酸盐生油岩中沥青变质程度和沥青热变质实验[J].地球化学,1982,42(3):237~243
    [3]
    Rogers M A,Mcalary J D,Bailey J L.Significance of reservoir bitumens to thermal-maturation studies,western Canada basin[J].AAPG Bull,1974,58(9):1806~1824
    [4]
    Jacob H.Classification,structure,genesis and practical importance of natural solid bitumen (migrabitumen)[J].International Journal of Coal Geology,1989,11:65~79
    [5]
    Hogg A J C,Hamilton P J,Macintyre R M.Mapping diagenetic fluid flow within a reservoir:K-Ar dating in the Alwyn area(UK North Sea )[J].Marine and Petroleum Geology,1993,10:279~294
    [6]
    Yen T F.In bitumen,Asphalts and Tar Sands[J].Elsevir,1978,13(2):1~15
    [7]
    吴征.鄂尔多斯盆地下奥陶统原生-同层沥青分析[J].天然气工业,1999,19(6):14~17
    [8]
    程克明.碳酸盐岩油气生成理论与实践[M].北京:石油工业出版社,1996.78~92
    [9]
    林峰,王廷栋.四川盆地碳酸盐岩储层中固体运移沥青的性质和成因[J].矿物岩石地球化学通报,1998,17(3):174~178
    [10]
    王建宝,郭汝泰,肖贤明等.塔里木盆地轮南低隆起早古生代油气藏形成的期次与时间研究[J].沉积学报,2002,20(2):320~325
    [11]
    金强.微量元素组成在固体沥青-源岩对比中的应用[J].石油实验地质,2001,23(3):285~290
    [12]
    肖贤明,刘德汉,傅家漠.沥青反射率作为烃源岩成熟度指标的意义[J].沉积学报,1991,9(增刊):138~146
    [13]
    肖贤明,刘德汉,傅家漠等.应用沥青反射率推算油气生成与运移的地质时间[J].科学通报,2000,45(19):2123~2127
    [14]
    徐世琦.加里东古隆起震旦-寒武系成藏条件[J].天然气工业,1999,19(6):7~10
    [15]
    李国辉,李翔,杨西南.四川盆地加里东古隆起震旦系气藏成藏控制因素[J].石油与天然气地质,2000,21(1):80~83
    [16]
    邓涛.四川盆地加里东隆起的构造机制和成藏模式[J].石油实验地质,1996,18(4):354~358
    [17]
    丰国秀,陈盛吉.岩石中沥青反射率与镜质组反射率之间的关系[J].天然气工业,1988,8(2):20~25
  • 加载中

Catalog

    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 (666) PDF downloads(387) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return