可控源音频大地电磁(csamt)在地热勘探中的应用

Jurnal Neutrino Pub Date : 2017-04-30 DOI:10.18860/neu.v9i2.4131

S. Susilawati, E. Mustopa

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摘要

可控源音频大地电磁是测定地表下岩石电阻率的地球物理学方法之一。CSAMT方法利用人工流并注入地下，人工源频率范围为0.1 Hz ~ 10 kHz，对CSAMT数据源效果进行反向校正。反演结果表明，该层的电阻率值在2.5 Ω之间。M - 15 Ω。M，这说明这一层是粘土。

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APPLICATION OF CONTROLLED SOURCE AUDIO MAGNETOTELLURIC (CSAMT) AT GEOTHERMAL

CSAMT or Controlled Source Audio-Magnetotelluric is one of the Geophysics methods to determine the resistivity of rock under earth surface. CSAMT method utilizes artificial stream and injected into the ground, the frequency of artificial sources ranging from 0.1 Hz to 10 kHz, CSAMT data source effect correction is inverted. From the inversion results showed that there is a layer having resistivity values ranged between 2.5 Ω.m – 15 Ω.m, which is interpreted that the layer is clay.

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Jurnal Neutrino

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