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新—甘地震测深剖面的地壳速度结构及大地构造单元划分
引用本文:徐新忠,王有学,蒋亚明,党淑娟,聂定平.新—甘地震测深剖面的地壳速度结构及大地构造单元划分[J].新疆地质,1992(2).
作者姓名:徐新忠  王有学  蒋亚明  党淑娟  聂定平
作者单位:地质矿产部第二综合物探大队 (徐新忠,王有学,蒋亚明,党淑娟),成都地质学院(聂定平)
摘    要:根据新—甘地震测深结果,以纵波为主,建立了剖面内地壳速度结构模型,结合横波资料对地壳结构进行了研究。确定出超壳断裂14条;划分出一级构造单元4个;二级构造单元8个。从而,对大地构造和地壳演化提出新的认识,为深入研究区内基础地质具有重要意义。

关 键 词:地震测深  地壳速度结构  断裂构造  地壳结构演化  构造单元划分

CRUSTAL VELOCITY STRUCTURE AND GEOTECTONIC UN|T DIVISION IN XINJIANG-GANSU SECTION BASED ON DEEP SEISMIC SOUNDING
Xu Xinzhong Wang Youxue Jiang Yamin Dang Shujuan.CRUSTAL VELOCITY STRUCTURE AND GEOTECTONIC UN|T DIVISION IN XINJIANG-GANSU SECTION BASED ON DEEP SEISMIC SOUNDING[J].Xinjiang Geology,1992(2).
Authors:Xu Xinzhong Wang Youxue Jiang Yamin Dang Shujuan
Abstract:The model of crustal velocity structure was established and the crustal structure was studied in the Gansu-Xinjiang section based on the data of deep seismic sounding, mainly of longitudinal wave. The analytic results show for-teen fractures cutting across the crust with four priliminary structural units and eight secondary structural units. Thus, the research presents new knowledge about geotectonics and crustal evolution, and has an important significance on the furture intensive study in this area.
Keywords:Deep seismic sounding  crustal velocity structure  fracturing structure  crustal structure evolution  tectonic unit division  
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