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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2008  >  30(2): 203-206
Bi Suping, Zhang Qinglong, Wang Liangshu, Chen Zhuxin, Xie Guoai, Xu Shiyin, Cui Yingbin. BALANCED CROSS-SECTION RESTORATION AND TECTONIC EVOLUTION ANALYSIS IN THE BINXIAN SAG, THE SONGLIAO BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(2): 203-206. doi: 10.11781/sysydz200802203
Citation: Bi Suping, Zhang Qinglong, Wang Liangshu, Chen Zhuxin, Xie Guoai, Xu Shiyin, Cui Yingbin. BALANCED CROSS-SECTION RESTORATION AND TECTONIC EVOLUTION ANALYSIS IN THE BINXIAN SAG, THE SONGLIAO BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(2): 203-206. doi: 10.11781/sysydz200802203
shu

BALANCED CROSS-SECTION RESTORATION AND TECTONIC EVOLUTION ANALYSIS IN THE BINXIAN SAG, THE SONGLIAO BASIN

doi: 10.11781/sysydz200802203
  • 1.

    Department of Earth Sciences, Nanjing University, Nanjing, Jiangsu 210093, China

  • 2. Research Institute of Petroleum Exploration and Development, Petro China, Beijing 100083, China

  • 3. Research Institute of Geological Sciences, Shengli Oil Field, SINOPEC, Dongying,Shandong 257015,China

  • Received Date: 2007-03-21
  • Rev Recd Date: 2008-01-30
  • Publish Date: 2008-03-28
    Abstract
  • Based on strata data analysis,with balanced cross-section technique,choosing 4 NS-trending cross-sections in the Binxian Sag in the east of Songliao Basin,seismic analysis sections are restored in this paper.Extension quantity,rate and velocity for each evolution stage are calculated.The Binxian Sag has experienced at least 4 evolution stages:fault,fault-depression,depression and tectonic inversion.Results have indicated that,extension velocities during the fault and fault-depression stages are higher,about 0.21 and 0.2 mm/a respectively.Deformation intensity in the center of Binxian sub-Sag is stronger than the margin.

     

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    • References(25)
  • [1]
    陈昭年,陈发景.松辽盆地反转构造运动学特征[J].现代地质,1996,10(3):390～396
    [2]
    解习农.中国东部中新生代盆地形成演化与深部过程的耦合关系[J].地学前缘,1998,5(增刊):162～165
    [3]
    陈发景,汪新文,张光亚等.中国中、新生代前陆盆地的构造特征和地球动力学[J].地球科学:中国地质大学学报,1996,21(4):366～372
    [4]
    刘翠荣,陈发景.裂谷盆地的理论模拟:以松辽盆地为例[J].石油实验地质,1996,18(3):274～282
    [5]
    张岳桥,赵越,董树文等.中国东部及邻区早白垩世裂陷盆地构造演化阶段[J].地学前缘,2004,11(3):123～133
    [6]
    李娟,舒良树.松辽盆地中、新生代构造特征及其演化[J].南京大学学报(自然科学版),2002,38(4):525～530
    [7]
    周荔青,吴聿元,张淮.松辽盆地断陷层系油气成藏的分区特征[J].石油实验地质,2007,29(1):11～16
    [8]
    吴聿元,周荔青.松辽盆地主要断陷大中型油气田形成分布特征[J].石油实验地质,2007,29(3):19～25
    [9]
    黑龙江省地质局区域地质测量队.1∶20万宾县幅(L-52-XX)区域地质测量报告[R].1967.8～180
    [10]
    贾军涛,王璞王君,张斌等.哈尔滨东宾县凹陷白垩纪地层层序及其与松辽盆地的对比[J].地质通报,2006,25(9-10):1143～1151
    [11]
    崔营滨.松辽盆地东缘宾县凹陷沉积特征与烃源岩初步评价[D] :[学位论文].西安:西北大学,2006
    [12]
    Gibbs A D.Balanced cross-section construction from seismic section in areas of extensional tectonics[J].Journal of Structural Geology,1983,5(2):153～160
    [13]
    薛冈,卢华复.伸展区域平衡剖面法及其在构造分析中的应用[J].高校地质学报,2001,7(4):428～433
    [14]
    漆家福,Groshong R H Jr.用面积平衡原理预测伸展断陷盆地中岩层内部应变及亚分辨正断层的方法[J].地球科学,2002,27(6):696～702
    [15]
    Woodward N B,Boyer S E,Suppe J.平衡剖面--地质研究与勘探工作的一种重要方法[M].贾维民,杜秀霞译.武汉:中国地质大学出版社,1991.1～140
    [16]
    佟彦明,钟巧霞.利用平衡剖面快速判定盆地区域古构造应力方向[J].石油实验地质,2007,29(6):103～106
    [17]
    周建勋.同沉积挤压盆地构造演化恢复的平衡剖面方法及其应用[J].地球学报,2005,26(2):151～156
    [18]
    Dahlstrom C D A.Balanced cross sections[J].Cannadian Journal of Earth Sciences,1969,(6):743～757
    [19]
    Schonborn G.Balancing cross sections with kinematic constraints:the dolomites(northern Italy)[J].Tectonics,1999,18(3):527～545
    [20]
    Dubey A K,Misra R,Bhakuni S S.Erratic shortening from balanced cross-sections of the western Himalayan foreland basin:causes and implications for basin evolution[J].Journal of Asian Earth Sciences,2001,19(6):765～775
    [21]
    Mukhopadhyay D K,Permanand M.A balanced cross section across the Himalayan frontal fold-thrust belt,Subathu area,Himachal Pradesh,India:thrust sequence,structural evolution and shortening[J].Journal of Asian Earth Sciences,2005 25(5):735～746
    [22]
    陈竹新,贾东,张惬等.龙门山前陆褶皱冲断带的平衡剖面分析[J].地质学报,2005,79(1):38～43
    [23]
    Zhou J X,Xu F Y,Wang T C,et al.Cenozoic deformation history of the Qaidam Basin,NW China:Results from cross-section restoration and implications for Qinghai-Tibet Plateau tectonics[J].Earth and Planetary Science Letters,2006,243:(1-2)195～210
    [24]
    颜丹平,田崇鲁,孟令波等.伸展构造盆地的平衡剖面及其构造意义--以松辽盆地南部为例[J].地球科学,2003,28(3):275～280
    [25]
    张树林,费琪,叶加仁.断陷盆地边缘凹陷类型及成因[J].石油实验地质,2007,29(1):47～51
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