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首页> 外文期刊>Arabian journal of geosciences >Detection of a thin layer by seismic reflection with different geophones at a site in Liangzhu, Southeastern China
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Detection of a thin layer by seismic reflection with different geophones at a site in Liangzhu, Southeastern China

机译:中国东南部良渚地震检测薄层用地震反射检测薄层

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摘要

Geophone properties are important factors for high-resolution seismic exploration and greatly influence the quality of data. In this study, we will address the problems of ultra-shallow seismic data acquisition and processing. The purpose of our study is to evaluate the applicability of using different seismic geophones and processing techniques to detect a thin soil layer that is approximately 20 cm in thickness at a depth of approximately 2 m in the Liangzhu archaeological site in southeastern China. We collected seismic data using two types of geophones: normal geophones with different natural frequencies inserted into the ground and towable cable geophones contacting the earth's surface. We considered combining the frequency advantages of these two different types of geophones to broaden the effective bandwidth of the acquired data. To achieve this, we designed a partial frequency match filtering method for data processing, which helps to improve the resolution of the reflected seismic data. The stacking profile results show that match filtering is effective in detecting a thin layer compared to drilling samples and GPR data the velocity of the thin bed is 350ms while from seismic section interval velocity of the contact between clayey soils and rammed sandy soils about 600 ms.
机译:地震孔属性是高分辨率地震勘探的重要因素,大大影响数据质量。在这项研究中,我们将解决超浅地震数据采集和处理的问题。我们研究的目的是评估使用不同地震性地震检波器和加工技术的适用性检测薄的土壤层,其厚度约为20厘米,深度在良渚考古地区在中国东南部的约2米。我们使用两种类型的地震孔收集地震数据:具有不同自然频率的正常地震检波器插入地面和可牵引电缆地震检波器接触地球表面。我们考虑结合这两种不同类型的地理位音的频率优势来扩大所获取数据的有效带宽。为此,我们设计了一种用于数据处理的部分频率匹配滤波方法,这有助于提高反射地震数据的分辨率。堆叠轮廓结果表明,与钻孔样品相比,匹配过滤有效地检测薄层,并且GPR数据薄床的速度为350ms,而粘土土壤和夯土晶体的地震截面间隔速度约为600毫秒。

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