几种地震折射法数据处理的统计分析:一个综合数据实例

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Geofizika Pub Date : 2017-01-01 DOI:10.15233/GFZ.2017.34.2
P. Adetokunbo, O. Sanuade, P. Edigbue, K. Adegbola, Toluwani Daramola
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引用次数: 3

摘要

延迟时间法由于具有绘制覆盖层横向厚度和基岩起伏的能力,在浅层地震折射测量中受到了广泛的关注。本研究利用合成数据对正负法和传统的互反法的性能进行了比较。用这两种方法得到的解释与实际地球物理模型相当。这表明,这两种方法都可以用来构造地质剖面。然而,随机完全块设计(RCBD)实验结果显示,所使用的方法类型存在显著差异,这需要进一步的试验。两两比较表明,正负法产生的模型比传统的倒数法更能模拟实际数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Statistical analysis of data processing in some seismic refraction methods: A synthetic data example
The delay time method has gained attention in shallow seismic refraction survey because it has the capability to map the lateral thickness of overburden and relief of bedrock. This study addresses the comparison between the performances of the plus-minus and conventional reciprocal methods using a synthetic data. The interpretations obtained from both methods are reasonably comparable to the actual geophysical models. This suggests that either of the methods can be used to construct a geologic section. However, the result of randomized complete block design (RCBD) experiment shows a significant difference in the type of method used and this necessitate the need for further test. The pairwise comparison suggests that the plus-minus method produces a model that better mimics the actual data than the conventional reciprocal method.
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来源期刊
Geofizika
Geofizika 地学-地球化学与地球物理
CiteScore
1.60
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: The Geofizika journal succeeds the Papers series (Radovi), which has been published since 1923 at the Geophysical Institute in Zagreb (current the Department of Geophysics, Faculty of Science, University of Zagreb). Geofizika publishes contributions dealing with physics of the atmosphere, the sea and the Earth''s interior.
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