李祥, 包东健, 陈原平, 束沛镒, 朱碚定. 内蒙古中部地区的壳幔介质分层结构[J]. 华北地震科学, 1987, 5(4): 58-65,84.
引用本文: 李祥, 包东健, 陈原平, 束沛镒, 朱碚定. 内蒙古中部地区的壳幔介质分层结构[J]. 华北地震科学, 1987, 5(4): 58-65,84.
Li Xiang, Bao Dongjian, Chen Yuanping, Su Peijian, Zhu Peiding. THE LAYERED STRUCTURE OF THE CURST AND MANTLE MEDIUM IN CENTRAL INNER MONGGOLIA[J]. North China Earthquake Sciences, 1987, 5(4): 58-65,84.
Citation: Li Xiang, Bao Dongjian, Chen Yuanping, Su Peijian, Zhu Peiding. THE LAYERED STRUCTURE OF THE CURST AND MANTLE MEDIUM IN CENTRAL INNER MONGGOLIA[J]. North China Earthquake Sciences, 1987, 5(4): 58-65,84.

内蒙古中部地区的壳幔介质分层结构

THE LAYERED STRUCTURE OF THE CURST AND MANTLE MEDIUM IN CENTRAL INNER MONGGOLIA

  • 摘要: 本文采用综合地震图与内蒙中部六个台的深源远震记录波形拟合的方法求得各台站区域的壳幔分层结构模型。结果表明,集宁台地域的介质模型与我国华北平原西北边缘相似,其地壳厚度约46公里,而百灵庙、乌兰花、呼和浩特、和林格尔和清水河五个台所在区域的地壳厚度约为54公里左右,并有高低波速相间的情况,这与我国西北、西南地区有类似之处。

     

    Abstract: The layered structure model of crust and mantle in the various station regions have been obtained by the way of fitting synthetic seismograms with waveform of deep focus telcseismic record of the six stations in central Inner Monggolia.The results have shown that the medium model of jining station region is similar to that of the northwest baundary of North China plain,whoes crustal thickness is about 46 km, The crustal thickness under ihe regions of Bailingmiao, Walanhua, HuhehaOte, Helingeer and Qingshuihe five stations are about 54 km,with alternate high velocity layer and low velocity layer,which is similar to the struetture in the northwest and the southwest areas of our country.

     

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