断层相关褶皱的几何学模型及其应用
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引用本文:陈剑,卢华复,于景宗,王胜利.2005.断层相关褶皱的几何学模型及其应用[J].地球学报,26(1):89-92.
DOI:10.3975/cagsb.2005.01.14
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作者单位E-mail
陈剑 中国科学院地质与地球物理研究所北京100029 cjian2002@sohu.com 
卢华复 南京大学地球科学系江苏南京210093  
于景宗 东堪一公司吉林通化134000  
王胜利 南京大学地球科学系江苏南京210093  
基金项目:国家自然科学基金项目(编号:49832040)
中文摘要:在前陆盆地逆冲带中发育两种主要的断层相关褶皱构造样式:断层转折褶皱和断层传播褶皱。利用断层相关褶皱的下伏断层和上覆褶皱之间的角度参数存在的函数关系,可以对自然构造横剖面的构造解释进行检验。由于在时间地震剖面下的构造图形由于产生变形而与实际的自然构造有一定的偏差,这会影响几何学模型检验的有效性,因此在应用的过程中需要进行校正。通过地震速度谱将时问地震剖面转化为深度地震剖面,然后利用几何学关系对断层相关褶皱的构造剖面进行了检验。
中文关键词:前陆盆地逆冲带  断层相关褶皱  断层转折褶皱  断层传播褶皱  几何学检验
 
Geometric Models of Fault-related Folds and Their Application
Abstract:There are two main types of fault-related folds in the foreland thrust belts, i. e. , fault-bending folds and fault-propagation-folds. Forthe brittle rock deformation, there exists quantitative geometric relationship between fault shape and fold shape. According to the specific angular function relationships of fault-related fold models, the natural geological structures and the interpretation of seismic sections can be analyzed and tested geometrically. Through examination of seismic-time sections it is found that the structure configurations always lose shapes from their natural structures, thus an effect on the validity of geometric tests will occur. The transformation from the seismic-time section into the seismic-depth section by seismic speed spectrum can be carried out to test the reasonabili-ty of the interpreted structures. The subsurface structure examples of the tests are given from the Tarim oil field in Kuqa basin. With the geometric analysis and tests of the subsurface structures, the authors have successfully interpreted and predicted the original existence of the fault-bending folds and fault-propagation folds in fault-related folds of Kuqa area.
keywords:foreland thrust belt  fault-related fold  fault-bending fold  fault-propogation fold  geometric test
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