processding59.pdf - page 31

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The -D Resistivity Survey Method Using for the Geological Structure Determination
of the Limestone in Tamot Sub-District, Tamot District, Phatthalung Province
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Phanusak Yokorach
1
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2*
, Suchane Prommuean
3
and Teeradach Yaibok
3
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ćĒïïǰ2D-ERI ēé÷Ĕßš
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üĒïïĕéēóúǰ– ĕéēóúǰìĊę
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Ö(n)ìĆĚ
ÜĀöéǰ17 ßĆĚ
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1.8 Öĉ
ēúđöêøǰēé÷ÿøš
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ü÷ēðøĒÖøöǰRES2DINV đüĂøŤ
ßĆę
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øą÷ąǰ0-450 đöêø đðŨ
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üÜǰ2,080–6,500ǰēĂĀŤ
öđöêøǰēé÷ìĊę
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øą÷ąǰ450-1,350 đöêø ÝąöĊ
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ǰ50–250ǰđöêø ĒúąîĂÖÝćÖîĊĚ
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Öðøąöćèǰ70-
200 đöêø Ă÷ĎŠ
ìĊę
øą÷ąǰ1,050-1,250 đöêø ×ĂÜĒîüÖćøÿĞ
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é×üćÜÿõćóêš
ćîĕôôŜ
ćĒïïǰ ǰöĉ
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ð×ïüî×ĆĚ
üĒïïĕéēóú–ĕéēóú
ǰǰ
Abstract
This study research is the geomorphological structure of the limestone in the area of Tamot
Sub-District, Tamot district, Phatthalung province. The electrical resistivity survey of 2D-ERI was used
by the diploe-dipole configuration with 50 m of the electrode spacing, 225 m of maximum depth for
17 levels and 1.8 km of the line survey length. The 2D-ERI model was simulated by RES2DINV v.4.05
program. The result was shown the geological structure of Quaternary and sedimentary rock with
profile along 0-450 m, reserved by the limestone with resistivity of 2,080 – 6,500 ņm. The limestone
out croup on 450-1,350 m of profile length was reserved by the granitic base rock at 50-250 m of
depth. Furthermore, the characterization of a cavity limestone was found at 70-200 m of depth, at the
range 1,050-1,250 m along the profile line.
Keyword:
Limestone, 2D Electrical Resistivity Image, Dipole-Dipole Electrode Configuration
1
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* Corresponding author: Tel.: 098-0163961. E-mail address:
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