首页> 外文会议>2011 2nd International Conference on Environmental Engineering and Applications >Non-invasive Geophysical Techniques for Prospecting the Sungai Batu Archaeological Site, Kedah, Malaysia
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Non-invasive Geophysical Techniques for Prospecting the Sungai Batu Archaeological Site, Kedah, Malaysia

机译:探寻双溪巴都考古遗址的非侵入性地球物理技术,马来西亚吉打

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A geophysical survey that involved two different techniques of seismic refraction and magnetic was carried out with the aim of locating buried artifacts and specifying subsurface geological properties in a non-invasive manner at the Sungai Batu archaeological site, Kedah, Malaysia. Sungai Batu archaeological area is considered by archaeologists as a high-potential archaeological area where scientists search for signs of civilization. Seismic refraction method was performed for two profiles with using a 24 channel seismograph. The processing of the seismic refraction data was based on the FIRSTPIX and GREMIX15 software. The seismic results indicated that the area is composed of two main layers: the upper layer, made up of soil consisting of alluvium and sandy clay, and the second layer, made up of mixed saturated soil with water. The magnetic survey was conducted using a G-856 proton precession magnetometer with 5m sampling interval along 10m spaced parallel survey lines over 15 profiles. Six significant anomalies were found from residual magnetic map which two anomalies had high magnetic values, which can be related to ruins of old buildings made of mud bricks. An excavation test, performed by archaeologists, confirmed the geophysical results. Consequently, the investigated results approved the usefulness of geophysical techniques in mapping the subsurface structure and buried artifacts to design a more efficient plan for reducing the prospecting time and minimizing the environmental damage of archaeological excavation.
机译:在马来西亚吉打州的双溪巴图考古现场,进行了涉及两种不同的地震折射和磁学技术的地球物理调查,目的是以非侵入性的方式定位埋藏的文物并指定地下地质特征。双溪巴都考古区被考古学家视为高潜力考古区,科学家们在这里寻找文明的迹象。使用24通道地震仪对两个剖面进行了地震折射法。地震折射数据的处理基于FIRSTPIX和GREMIX15软件。地震结果表明,该区域由两个主要层组成:上层是由冲积层和沙质粘土组成的土壤,第二层是由饱和饱和土和水混合而成的。磁力测量是使用G-856质子旋进磁力仪进行的,采样间隔为5m,沿着15m剖面上10m平行的平行测量线。从剩余磁图中发现了六个显着异常,其中两个异常具有较高的磁值,这可能与用泥砖​​建造的老建筑的废墟有关。考古学家进行的挖掘测试证实了地球物理结果。因此,研究结果证实了地球物理技术在测绘地下结构和埋藏的文物方面的有用性,以设计一种更有效的计划,以减少勘探时间并最大程度地减少考古发掘对环境的破坏。

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