Huang Zeguang, Gao Changlin. BASIN SEQUENCE AND OIL-GAS POTENTIAL IN NEAR NORTHERN QINLING-DABIE MOUNTAIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(1): 25-31. doi: 10.11781/sysydz200701025
Citation: Huang Zeguang, Gao Changlin. BASIN SEQUENCE AND OIL-GAS POTENTIAL IN NEAR NORTHERN QINLING-DABIE MOUNTAIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(1): 25-31. doi: 10.11781/sysydz200701025

BASIN SEQUENCE AND OIL-GAS POTENTIAL IN NEAR NORTHERN QINLING-DABIE MOUNTAIN

doi: 10.11781/sysydz200701025
  • Received Date: 2006-01-09
  • Rev Recd Date: 2006-12-05
  • Publish Date: 2007-01-28
  • There are lots of basins which have contained some oil gas in near northern Qinling-Dabie mountain.The geological-geochemical research results showed that there are 6 basin generations in near northern QinlingDabie mountain: 1)passive continental margin basin(C1-O2),2)back-arc basin(O2-C1),3)residual basin(C2-T2),the stage 1(C2-P12) and stage 2(P12-T2),4)intracontinental foreland basin(T3-J2),5)extensional strike-slip basin(J3-K1),6)fault-depression basin(K2-E).Six source rock suites have been developed,Eogene system,Lower Cretaceous,Lower Jurassic,Upper Triassic,Carboniferous-Permian and Lower Palaeozoic in near northern Qinling-Dabie mountain.The main prospecting strata are Carboniferous-Permian,Lower Cretaceous,Upper Triassic and Eogene system in near northern Qinling-Dabie mountain.The Zhoukou Basin,Jiyuan Basin and Lao-Yi Basin are chosen as prospect.The Tanzhuang-Shenqiu Sag,Niqiuji Sag,Xiangcheng Sag,Wuyang Sag,Mengxian-Wenxian Sag and Luoyang Sag are chosen as favourite district.

     

  • loading
  • [1]
    张功成,王定一,吕锡敏.南华北中、新生代盆地构造特征[A].见:张功成,徐宏主编.中国含油气盆地构造[M].北京:石油工业出版社,1999.201~212
    [2]
    胡居文.华北地区中生代盆地与油气[J].石油与天然气地质,1989,10(4):378~391
    [3]
    袁政文,何明喜,宋建华等.周口残留盆地油气勘探前景分析[J].石油实验地质,2004,25(6):679~684
    [4]
    何明喜.东秦岭(河南部分)新生代拉伸造山作用与盆岭伸展构造[M].西安:西北大学出版社,1995.53~116
    [5]
    孙肇才.板内形变与晚期成藏[M].北京:地质出版社,2003.43~50
    [6]
    张渝昌.中国含油气盆地原型分析[M].南京:南京大学出版社,1997.1~450
    [7]
    戴金星,王庭斌,宋岩等.中国大中型天然气田形成条件与分布规律[M].北京:地质出版社,1997.1~300
    [8]
    田在艺,张庆春.中国含油气盆地岩相古地理与油气[M].北京:地质出版社,1997
    [9]
    张国伟,张本仁,袁学诚等.秦岭造山带与大陆动力学[M].北京:科学出版社,2000.1~854
    [10]
    吉让寿,秦德余,高长林等.东秦岭造山带与盆地[M].西安:西安地图出版社,1997.1~197
    [11]
    孙万禄,陈召佑,陈霞等.中国煤层气盆地地质特征与资源前景[J].石油与天然气地质,2005,26(2):141~146
    [12]
    任纪舜,王作勋,陈炳蔚等.从全球看中国大地构造:中国及邻区大地构造图简要说明[M].北京:地质出版社,2000.1~74
    [13]
    王鸿祯,杨森楠,刘本培.中国及邻区大地构造划分和构造发展阶段[A].见:王鸿祯主编.中国及邻区构造古地理和生物古地理[M].武汉:中国地质大学出版社,1990.3~34
    [14]
    任战利.中国北方沉积盆地热演化史对比[J].石油与天然气地质,2000,21(1):33~37
    [15]
    谈彩萍,刘翠荣.中国东部老油区油气成藏特征[J].石油实验地质,2005,27(2):144~150
    [16]
    曹高社,李学田,刘德良等.合肥盆地与北淮阳构造带印支期的推覆构造及其油气意义[J].石油与天然气地质,2003,24(2):116~122
    [17]
    吕俊祥,黄泽光.南华北地区中新生代盆地成盆环境分析[J].石油实验地质,2005,27(2):118~123
    [18]
    孙晓猛,张梅生,龙胜祥等.秦岭-大别造山带北部逆冲推覆构造与合肥盆地、周口坳陷控盆断裂[J].石油与天然气地质,2004,25(2):191~199
    [19]
    高长林,叶德燎,钱一雄.前陆盆地的类型及油气远景[J].石油实验地质,2000,22(2):99~104
    [20]
    刘文灿,王果胜.北淮阳地区中生代逆冲推覆构造[J].现代地质,1999,13(2):143~149
    [21]
    黄泽光,高长林,吉让寿.南华北地区中新生代盆地演化[J].石油与天然气地质,2005,26(2):252~256
    [22]
    许长海,周祖翼,马昌前等.大别造山带140~85 Ma热窿伸展作用:年代学约束[J].中国科学(D辑),2001,31(11):925~937
    [23]
    杨坤光,马昌前,许长海等.北淮阳构造带与大别造山带的差异性隆升[J].中国科学(D辑),1999,29(2):97~103
    [24]
    周新科,许化政.豫西地区晚三叠世原型盆地及含油气性分析[J].石油实验地质,2005,27(3):211~217
    [25]
    全书进.周口坳陷上古生界油气资源潜力分析[J].石油实验地质,2004,26(6):542~546
    [26]
    许世红.安参1井侏罗系和石炭-二叠系暗色泥岩地球化学特征及意义[J].石油实验地质,2002,24(3):284~286
    [27]
    曹高社.合肥盆地中--新生界烃源岩地球化学与构造背景分析[J].石油实验地质,2004,26(3):287~291
  • 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 (703) PDF downloads(303) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return