CAJ | 학술논문

针对核电工程选址中的能动断层地质调查工作需要, 提出了利用共偏移距浅层地震反射时间剖面来拓展地质剖面解释深度的技术方法, 通过物性和岩性的综合解释来提高对能动断层鉴别及其产状确定的可靠性. 探测试验结果表明该方法是有效可行的. 地质剖面上描述的断裂破碎带在共偏移距时间剖面上反应明显, 二者可以相互印证, 优势互补. 该技术方法可用于类似工程地质调查和第四系覆盖较薄地区的隐伏断层探测.
침대핵전공정선지중적능동단층지질조사공작수요, 제출료이용공편이거천층지진반사시간부면래탁전지질부면해석심도적기술방법, 통과물성화암성적종합해석래제고대능동단층감별급기산상학정적가고성. 탐측시험결과표명해방법시유효가행적. 지질부면상묘술적단렬파쇄대재공편이거시간부면상반응명현, 이자가이상호인증, 우세호보. 해기술방법가용우유사공정지질조사화제사계복개교박지구적은복단층탐측.
In order to meet the needs of capable fault geological survey on nuclear power project sites, this paper proposes a technical method of using common-offset shallow seismic reflection profiles to extend the interpretation depth of geological cross-sections. Through comprehensive interpretation of the physical properties and lithology, the identification of capable faults and determination of their attitude can be more reliable. The test results show that the method is effective and feasible. The fracture zones found on geological profiles are also visible on the common-offset shallow seismic reflection profiles. The geological and seismic interpretations may verify each other. The technical approach provided by this paper can be applied to similar engineering geological investigations, and also to buried fault detection in a thin Quaternary covered area.