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浅层地震折射波法综述

An overview of shallow seismic refraction methods

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【作者】 赵德亨田钢王帮兵

【Author】 ZHAO De-heng1,3 , TIAN Gang2 , WANG Bang-bing11. College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, Jilin, China 2. Department of Earth Sciences, College of Science, Zhejiang University, Hangzhou 310027, Zhejiang, China 3. Department of Geology, Sariwon University of Geosciences, Pyongyang, D.P.R. Korea

【机构】 吉林大学地球探测科学与技术学院浙江大学理学院地球科学系吉林大学地球探测科学与技术学院 吉林长春130026 沙里院地质大学地质系平壤朝鲜浙江杭州310027吉林长春130026

【摘要】 浅层地震折射波法是在工程地质、水文地质及环境地质勘查中广泛应用的地震探测方法之一。在工程地质调查中,根据不同的场地地质条件和勘察目的,合理地正确应用浅层折射波法可以取得较明显的岩土工程勘察效果。本文简要地回顾了浅层地震折射法的发展历史,对各种新近发展的折射波解释方法进行了简单的介绍和比较,并列举了工程勘察中的应用领域。

【Abstract】 The shallow seismic refraction method is one of the main methods of exploration for engineering,hydrogeological and environmental geology. According to the different geological conditions and investigation purposes in engineering geological investigation,with right application of the reasonable seismic refraction method,more obvious result of geotechnical engineering survey can be gained. This paper briefly looked back to the developing history of shallow seismic refraction method and carried on the simple introduction and comparison of various update interpretation methods. It presented some applied fields in engineering geologic investigation by the seismic refraction method.

  • 【分类号】P631.4
  • 【被引频次】44
  • 【下载频次】1237
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