杨承先. 太原盆地晚古生代同生断裂的揭示及其地质意义[J]. 煤田地质与勘探, 1989, 17(4): 30-31.
引用本文: 杨承先. 太原盆地晚古生代同生断裂的揭示及其地质意义[J]. 煤田地质与勘探, 1989, 17(4): 30-31.

太原盆地晚古生代同生断裂的揭示及其地质意义

  • 摘要: 地震探测表明,太原盆地基底存在一条主干断裂。据地层资料分析,该断裂为石炭二叠纪的同生断裂或生长断裂,说明华北晚古生代地壳不仅有垂直运动,而且有水平运动。

     

    Abstract: Based on the consideration of engineering geological factors such as construction of coal field,characters of bedding and rock groups,variable characteristy of lithology, quality gradation of rock mass, variable characteristy of construction, the effects discharge river valley and the analysis of hydrogeologic condition etc,this paper presents and method,named mlti-factor engineering geological analysis.

     

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