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Geophysical Applications in Mapping theSubsurface Structure of Archaeological Site atLembah Bujang, Kedah, Malaysia

机译:在马来西亚考古布局考古遗址映射结构中的地球物理应用

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Lembah Bujang is one of Peninsular Malaysia's most important areas for archaeology as excavations in this area have revealed many traces of Malaysia's prehistory. The site is one of the oldest known place human activities the Peninsula. The aim of this study is to map and understand the subsurface structure of the survey area which is one of the archaeologically interesting areas. Geophysical methods are used because it is nondestructive and do not disturb the site. The methods are relatively quick and the results are used as a guide for subsequent excavation work. So it can greatly help in setting the digging priorities as geophysical surveying can reveal, for instance, important subsurface features like monuments, tunnels, voids, or buried walls. The geophysical methods used in this study were the magnetic gradiometer, 2-D electrical resistivity and ground penetrating radar (GPR) method. The integration of these three methods can be beneficial as each method has its strength and limitation. The specific area of study is in Sungai Batu and the results show that the sedimentation consists of sandy clay, alluvium and boulders with a depth of between 0 m to 15m.
机译:Lembah Bujang是半岛马来西亚最重要的考古地区,因为这一领域的挖掘揭示了许多马来西亚史前的痕迹。该网站是半岛最古老的人类活动之一。本研究的目的是映射和理解调查区域的地下结构,这是一个考古学上有趣的区域之一。使用地球物理方法,因为它是非破坏性的,并且不会打扰该网站。该方法相对较快,结果用作后续挖掘工作的指导。因此,它可以极大地帮助将挖掘优先级设置为地球物理测量可以揭示,例如,重要的地下功能,如纪念碑,隧道,空隙或埋地墙。本研究中使用的地球物理方法是磁梯度计,2-D电阻率和地面穿透雷达(GPR)方法。这三种方法的整合可能是有益的,因为每种方法都有其强度和限制。特定的学习领域是Sungai Batu,结果表明,沉降包括砂质,加油和巨石,深度为0米至15米。

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