Distinction of the Type of Mudstone at Bukt Chondong, Perlis Using 2-D Resistivity Method

N. Muztaza, N. A. Nawawi, M. T. Zakaria, T. Adeeko
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Abstract

Summary The study explores the use of 2-D resistivity method to identify the type of mudstone from the outcrop of Bukit Chondong (BC), Perlis. The distinction of mudstone is based from the comparison of resistivity values of different mudstone, which are the red mudstone and the grey mudstone from outcrop of Guar Jentik (GJ) and Utan Aji (UA) in Perlis. All the survey outcrops was identified within the same classification of Kubang Pasu Formation. The resistivity survey was performed using SAS4000 Terrameter with Pole-dipole array configuration. The resistivity was implemented on a single 40 m survey line with minimum 1 m electrode spacing. The resistivity data was processed by utilizing RES2DINV and Surfer 10 software which the inversion results was displayed in a form of contouring values. The range of resistivity value for red mudstone is 10 to 150 Ωm and grey mudstone is 120 to 500 Ωm. The resistivity value for mudstone of BC is 20 to 130 Ωm, which fall in the range values of red mudstone. Thus, mudstone of BC has the possible to be classified as red mudstone.
用二维电阻率法判别波斯北川洞泥岩类型
本研究利用二维电阻率法对Perlis Bukit Chondong (BC)露头泥岩类型进行了识别。通过对比不同泥岩的电阻率值进行泥岩的区分,分别是在Perlis Guar Jentik (GJ)和Utan Aji (UA)露头的红色泥岩和灰色泥岩。所有的露头都被确定在库邦帕苏组的同一分类中。电阻率测量采用SAS4000 Terrameter,采用极-偶极阵列配置。电阻率测量是在一条40米的测量线上进行的,电极间距最小为1米。利用RES2DINV和Surfer 10软件对电阻率数据进行处理,反演结果以等值线形式显示。红色泥岩的电阻率值范围为10 ~ 150 Ωm,灰色泥岩的电阻率值范围为120 ~ 500 Ωm。BC泥岩的电阻率值为20 ~ 130 Ωm,落在红色泥岩的范围内。因此,BC泥岩有可能被归类为红色泥岩。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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