Study of Sedimentary Outcrop of Semanggol Formation with the Correlation of Geology, Geotechnical and Geophysics Technique

Southeast Asian Conference on Geophysics

Nordiana, A.N.^1 ; Nordiana, M.M.^1 ; Ying Jia, Teoh^1 ; Hisham, Hazrul^1 ; Sulaiman, Nabila^1 ; Maslinda, Umi^1 ; Taqiuddin, Z.M.^1 ; Nur Amalina, M.K.A.^1 ; Afiq Saharudin, Muhamad^1

School of Physics, Universiti Sains Malaysia, Penang

11800, Malaysia^1

关键词: 2-D resistivities;    Electrode spacing;    Geophysical methods;    Geotechnical tests;    Good correlations;    Ground penetrating radar (GPR);    Resistivity methods;    Wenner schlumberger;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/62/1/012013/pdf
DOI  :  10.1088/1755-1315/62/1/012013

来源: IOP

【 摘 要 】

The study location was at Bukit Kukus, Kuala Ketil, Kedah, Malaysia where the geological outcrop of this Semanggol Formation comprises of chert, mudstone, and volcanic tuff. The study was conducted using two geophysical methods, which are 2-D Resistivity and Ground Penetrating Radar (GPR). The objectives of the study are to correlate both of the geophysical methods through the value of conductivity and to identify the physical properties of rocks through the value of porosity and permeability. The data acquisition for both methods was conducted on the same line. For 2-D Resistivity method, the length of the line is 60 m with 1.5 m electrode spacing and the array used was Wenner-Schlumberger. For GPR method, the survey line was on top of the resistivity line, and the frequency of the antenna used is 250 MHz. A good correlation exists between both of the GPR signature and contour maps for resistivity from the surfer 10 software with the outcrop feature. Conductivity value from both GPR and Resistivity method was compared and the range value of conductivity obtained from GPR method almost equivalent with Resistivity method based on derivation and calculation for the sedimentary rocks, which are 0.037 to 0.574 miliSiemens per metre (mS/m) for chert and 0.186 to 10.142 miliSiemens per metre (mS/m) for mudstone. Two types of rock samples were taken, and several geotechnical tests were conducted, but only the value of permeability, K and porosity, of chert can be calculated, which are 1.95E-22 m2(original condition) and 2.27E-22 m2(dry condition) and 3 percent respectively as the sample of mudstone was damaged. The parameter of the 2-D resistivity method derived from Archie's law was used to calculate the porosity,fvalue using the Formation Factor equation. The range values of porosity,ffor chert mostly in the range of 5 to 25 percent, which is 6.26 to 13.36 percent but slightly out of range for mudstone, which is 14.12 to 36.02 percent.