自相似性在遥感构造研究中的应用
|
摘要
通过对韧性剪切带中区域构造、小型构造和显微构造的对比,证明这3种样式的构造在几何学和运动学方面具有相似性,进而采用分形理论,利用显微构造和小型构造的研究方法,借助遥感技术对东天山地区的大型韧性剪切带进行了应变分析。经与前人研究结果对比,说明显微构造的研究方法适用于遥感区域构造分析。分形理论与遥感技术相结合将是遥感地质的发展方向。
Regional tectonics,small-scale structures and microstructures in the ductile shearing zone are proved to be similar to each other in geometry and kinematics by comparing their patterns,so the methods for studying microstructures were used to the strain analysis in a ductile shearing zone in East Tianshan region with the aid of remote sensing.According to the theory of fractal,the methods for studying microstructures are suitable for the study of regional tectonics,as evidenced by their comparison with existing achievements.The combination of fractal with remote sensing might be a new development direction in geological survey.
Regional tectonics,small-scale structures and microstructures in the ductile shearing zone are proved to be similar to each other in geometry and kinematics by comparing their patterns,so the methods for studying microstructures were used to the strain analysis in a ductile shearing zone in East Tianshan region with the aid of remote sensing.According to the theory of fractal,the methods for studying microstructures are suitable for the study of regional tectonics,as evidenced by their comparison with existing achievements.The combination of fractal with remote sensing might be a new development direction in geological survey.
引文
[1]Mandelbrot B.How Long is the Coast of Britain?Statistical Self-Similarity and Fractional Dimension[J].Science,1967(156):636-638.
[2]Mandelbrot B.Fractal:Form,Chance and Dimension[M].San-Francisco:W.H.Freeman,1977:1-10.
[3]Barnsley M F.Fractals Everywhere[M].Boston:Academic PressProfessional,1993:63-67.
[4]Turcotte D L.Fractals and Chaos in Geology and Geophysics[M].Cambridge Uni.Press,1992:38-41.
[5]Agterberg F P.Multifractal Simulation of Geochemical Map Pat-terns[M]//Merriam D F,Davis J C.Geologic Modeling andSimulation:Sedimentary Systems.NewYork:Kluwer,2001:327-346.
[6]於崇文.成矿动力系统在混沌边缘分形生长——一种新的成矿理论与方法论(上)[J].地学前缘,2001(3):9-28.
[7]於崇文.成矿动力系统在混沌边缘分形生长——一种新的成矿理论与方法论(下)[J].地学前缘,2001(4):471-489.
[8]於崇文.地质系统的复杂性——地质科学的基本问题(I)[J].地球科学,2002,27(5):509-519.
[9]赵鹏大.地质异常理论与矿床预测:现代矿产资源评价理论与方法[M].北京:地质出版社,1998:3-11.
[10]成秋明.空间模式的广义自相似性分析与矿产资源评价[J].地球科学,2004,29(6):733-744.
[11]成秋明.成矿过程奇异性与矿产预测定量化的新理论与新方法[J].地学前缘,2007(5):42-53.
[12]Zhou YZ,Chown E H,Tu G Z.Geochemical Migration and Result-ant Distribution Patterns of Impurity Trace Elements in SourceRocks[J].Mathematical Geology,1994(4):419-435.
[13]谢淑云,成秋明,李增华,等.矿物微观结构的多重分形[J].地球科学,2009(2):264-269.
[14]夏勇,赵荣椿.基于形态学多重分形的遥感图像多尺度分割[J].计算机应用,2006(9):2072-2073.
[15]王倩,陈建平.基于分形理论的遥感蚀变异常提取和分级[J].地质通报,2009(Z1):285-288.
[16]张建东,彭省临,杨斌,等.分形理论在云南个旧锡矿遥感信息定量化分析中的应用[J].地质找矿论丛,2008(2):65-68.
[17]谢和平.分形应用中的数学基础与方法[M].北京:科学出版社,1997:8-23.
[18]陈颙,陈凌.分形几何学[M].北京:地震出版社,2005:5-17.
[19]李德伦,王恩林.构造地质学[M].长春:吉林大学出版社,2001:200-201.
[20]杨兴科,张连昌,姬金生,等.东天山秋格明塔什—黄山韧性剪切带变形特征分析[J].西安工程学院学报,1998,20(3):11-18.
[21]刘颖,刘刚.显微构造研究方法在韧性剪切带遥感分析中的应用[J].吉林大学学报(地球科学版),2010,40(3):508-515.
[22]徐兴旺,马天林,孙立倩,等.新疆觉罗塔格韧性变形带组构及动力学意义[J].地质力学学报:1998,4(1):25-32.
[23]徐兴旺,马天林,张学勤,等.新疆东天山觉罗塔格韧性挤压带基本特征及动力学意义[J].地质科学,1998,33(2):147-157.
[24]Wang Yu,Li Jinyi,Sun Guihua.Postcollisional Eastward Extru-sion and Tectonic Exhumation along the Eastern Tianshan Orogen,Central Asia:Constraints from Dextral Strike-Slip Motion and40Ar/39Ar Geochronological Evidence[J].The Journal of Geolo-gy,2008,116(6):599-618.
[2]Mandelbrot B.Fractal:Form,Chance and Dimension[M].San-Francisco:W.H.Freeman,1977:1-10.
[3]Barnsley M F.Fractals Everywhere[M].Boston:Academic PressProfessional,1993:63-67.
[4]Turcotte D L.Fractals and Chaos in Geology and Geophysics[M].Cambridge Uni.Press,1992:38-41.
[5]Agterberg F P.Multifractal Simulation of Geochemical Map Pat-terns[M]//Merriam D F,Davis J C.Geologic Modeling andSimulation:Sedimentary Systems.NewYork:Kluwer,2001:327-346.
[6]於崇文.成矿动力系统在混沌边缘分形生长——一种新的成矿理论与方法论(上)[J].地学前缘,2001(3):9-28.
[7]於崇文.成矿动力系统在混沌边缘分形生长——一种新的成矿理论与方法论(下)[J].地学前缘,2001(4):471-489.
[8]於崇文.地质系统的复杂性——地质科学的基本问题(I)[J].地球科学,2002,27(5):509-519.
[9]赵鹏大.地质异常理论与矿床预测:现代矿产资源评价理论与方法[M].北京:地质出版社,1998:3-11.
[10]成秋明.空间模式的广义自相似性分析与矿产资源评价[J].地球科学,2004,29(6):733-744.
[11]成秋明.成矿过程奇异性与矿产预测定量化的新理论与新方法[J].地学前缘,2007(5):42-53.
[12]Zhou YZ,Chown E H,Tu G Z.Geochemical Migration and Result-ant Distribution Patterns of Impurity Trace Elements in SourceRocks[J].Mathematical Geology,1994(4):419-435.
[13]谢淑云,成秋明,李增华,等.矿物微观结构的多重分形[J].地球科学,2009(2):264-269.
[14]夏勇,赵荣椿.基于形态学多重分形的遥感图像多尺度分割[J].计算机应用,2006(9):2072-2073.
[15]王倩,陈建平.基于分形理论的遥感蚀变异常提取和分级[J].地质通报,2009(Z1):285-288.
[16]张建东,彭省临,杨斌,等.分形理论在云南个旧锡矿遥感信息定量化分析中的应用[J].地质找矿论丛,2008(2):65-68.
[17]谢和平.分形应用中的数学基础与方法[M].北京:科学出版社,1997:8-23.
[18]陈颙,陈凌.分形几何学[M].北京:地震出版社,2005:5-17.
[19]李德伦,王恩林.构造地质学[M].长春:吉林大学出版社,2001:200-201.
[20]杨兴科,张连昌,姬金生,等.东天山秋格明塔什—黄山韧性剪切带变形特征分析[J].西安工程学院学报,1998,20(3):11-18.
[21]刘颖,刘刚.显微构造研究方法在韧性剪切带遥感分析中的应用[J].吉林大学学报(地球科学版),2010,40(3):508-515.
[22]徐兴旺,马天林,孙立倩,等.新疆觉罗塔格韧性变形带组构及动力学意义[J].地质力学学报:1998,4(1):25-32.
[23]徐兴旺,马天林,张学勤,等.新疆东天山觉罗塔格韧性挤压带基本特征及动力学意义[J].地质科学,1998,33(2):147-157.
[24]Wang Yu,Li Jinyi,Sun Guihua.Postcollisional Eastward Extru-sion and Tectonic Exhumation along the Eastern Tianshan Orogen,Central Asia:Constraints from Dextral Strike-Slip Motion and40Ar/39Ar Geochronological Evidence[J].The Journal of Geolo-gy,2008,116(6):599-618.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心