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Information Journal Paper

Title

1D AND 2D INTERPRETATION OF MT DATA IN THE EAST OF ALAGOL LAKE, GOLESTAN PROVINCE

Pages

  7-18

Abstract

 In this paper we study the subsurface down to 1300 m in the east of ALAGOL LAKE, located in the north of Golestan province, Iran. Geological structures according to the lithology, porosity and fluids have different responses to ELECTRIC AND MAGNETIC FIELDS. The layers containing salty water have high electric conductivity. The formation is Quaternary geological consists of jammed sediments. According to 1D and 2D models, three conductive layers were distinguished at the depths of 20 m to 90 m, 110 m to 500 m and about 1100 m. The last two layers are interpreted as the layers which consist of salty water. To prove the correctness of the results the 1D model of the MT data are compared with the results of a log record that is located at 4 Km southwestern of station B51.

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  • Cite

    APA: Copy

    SEDAGHAT, RABEA, & OSKOOI, BEHROOZ. (2011). 1D AND 2D INTERPRETATION OF MT DATA IN THE EAST OF ALAGOL LAKE, GOLESTAN PROVINCE. JOURNAL OF THE EARTH, 6(19), 7-18. SID. https://sid.ir/paper/192946/en

    Vancouver: Copy

    SEDAGHAT RABEA, OSKOOI BEHROOZ. 1D AND 2D INTERPRETATION OF MT DATA IN THE EAST OF ALAGOL LAKE, GOLESTAN PROVINCE. JOURNAL OF THE EARTH[Internet]. 2011;6(19):7-18. Available from: https://sid.ir/paper/192946/en

    IEEE: Copy

    RABEA SEDAGHAT, and BEHROOZ OSKOOI, “1D AND 2D INTERPRETATION OF MT DATA IN THE EAST OF ALAGOL LAKE, GOLESTAN PROVINCE,” JOURNAL OF THE EARTH, vol. 6, no. 19, pp. 7–18, 2011, [Online]. Available: https://sid.ir/paper/192946/en

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