Tong Yanming, Zhong Qiaoxia. FAST DETERMINATION OF BASIN'S PALEO-TECTONIC STRESS DIRECTION BY BALANCED CROSS SECTION——A NEW METHOD TO ANALYZE PALEO -TECTONIC STRESS DIRECTION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(6): 633-636. doi: 10.11781/sysydz200706633
Citation: Tong Yanming, Zhong Qiaoxia. FAST DETERMINATION OF BASIN'S PALEO-TECTONIC STRESS DIRECTION BY BALANCED CROSS SECTION——A NEW METHOD TO ANALYZE PALEO -TECTONIC STRESS DIRECTION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(6): 633-636. doi: 10.11781/sysydz200706633

FAST DETERMINATION OF BASIN'S PALEO-TECTONIC STRESS DIRECTION BY BALANCED CROSS SECTION——A NEW METHOD TO ANALYZE PALEO -TECTONIC STRESS DIRECTION

doi: 10.11781/sysydz200706633
  • Received Date: 2006-09-06
  • Rev Recd Date: 2007-10-24
  • Publish Date: 2007-11-28
  • To determine the direction of paleo-tectonic stress is a very important matter for basin's paleo-tectonic stress field research.A new method has been brought forward to analyze paleo-tectonic stress direction.Firstly,the balanced cross section technique is applied to obtain basin's deformation rates in different directions during each geological stage.Then,the strain rosette method is employed to calculate principal stress direction in mechanics of materials.Further,basin's deformation rates in 3 different directions are equated with strain rosette's linear strains.At last,basin's paleo-tectonic stress directions are figured out using the relevant formulae from mechanics of materials.The directions of the 1st extensional principal stress during Laiyang,Qingshan and Wangshi stages in the Jiaolai Basin have been obtained by this method,approximately NE-SW,NW-SE and S-N respectively.These results accord with those from other traditional geological methods,illustrating the feasibility of the new method.Besides,the changing trend of deformation rates in sections with different directions can reflect basin's mechanical property,so this method is also helpful for analyzing basin type and basin-forming mechanism.Obviously,this new method is convenient and can fast produce results,and is not restricted by strata outcrop condition.

     

  • loading
  • [1]
    万天丰.构造应力场研究的新进展[J].地学前缘,1995,2(1-2):226~235
    [2]
    许浚远,王艳萍,王磊等.多轴水平拉伸盆地三维古构造重建探讨[J].石油与天然气地质,1997,18(1):1~6
    [3]
    梁慧社,张建珍,夏义平.平衡剖面及其在油气勘探中的应用[M].北京:地震出版社,2002.2~3
    [4]
    邓承仪,成培江.工程材料力学实验[M].北京:科学技术文献出版社,1997.129~132
    [5]
    陆克政,戴俊生,陈书平等.胶莱盆地的形成及演化[M].东营:石油大学出版社,1994.33~144
    [6]
    刘华,李凌,吴智平.胶莱盆地烃源岩分布及有机地球化学特征[J].石油实验地质,2006,28(6):576~585
    [7]
    李桂群,范德江.胶莱盆地构造单元划分及其特征[J].青岛海洋大学学报,1994,24(2):239~246
    [8]
    胜利油田石油地质志编写组.中国石油地质志(卷六)胜利油田[M].北京:石油工业出版社,1993.491~505
    [9]
    翟慎德.胶莱盆地形成演化与油气形成条件[D]:[学位论文].广州:中国科学院广州地球化学研究所,2003
    [10]
    毛小平,吴冲龙,袁艳斌.地质构造的物理平衡剖面法[J].地球科学,1998,23(2):167~170
    [11]
    关康,罗镇宽,苗来成等.胶东招掖郭家岭型花岗岩锆石SHRIMP年代学研究[J].地质科学,1998,33(3):318~328
    [12]
    关康,罗镇宽,苗来成等.郭家岭型花岗岩地球化学特征与金矿化的关系[J].地质找矿论丛,1997,12(4):1~8
    [13]
    戴俊生,陆克政,宋全友等.胶莱盆地的运动学特征[J].石油大学学报(自然科学版),1995,19(2):1~6
    [14]
    Zhang Y Q,Dong S W,Shi W.Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province,eastern China[J].Tectonophysics,2003,363:243~258
    [15]
    施炜,张岳桥,董树文等.山东胶莱盆地构造变形及形成演化:以王氏群和大盛群变形分析为例[J].地质通报,2003,22(5):325~334
  • 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 (853) PDF downloads(440) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return