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Information Journal Paper

Title

Interpretation of Magnetic Anomalies in Astmal Area using the Largest Eigenvalue

Pages

  127-136

Abstract

 Summary Edge detection of causative bodies is crucial in interpretation of potential field data. Among the various edge detection methods, eigenvalue methods are majorly used to discriminate the gravity anomalies. The present investigation is, however, about to employ the eigenvalue methods to detect the magnetic anomalies. To this end, The largest eigenvalue method was applied to the total intensity of the magnetic data in Astmal area besides the vertical derivative, tilt angle and analytical signal methods in order to interpret the magnetic anomalies. In aids of the mentioned methods, the Geomagnetic target map was prepared and integrated with the geological information. Results indicated that the mineralizing fluids infiltrate the faults and fractures of the area. Also, dykes might play important roles in formation of the Astmal magnetite deposit...

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    APA: Copy

    Zareie, Vahid, & HAMIDZADEH MOGHADAM, RASOUL. (2019). Interpretation of Magnetic Anomalies in Astmal Area using the Largest Eigenvalue. JOURNAL OF RESEARCH ON APPLIED GEOPHYSICS, 5(1 ), 127-136. SID. https://sid.ir/paper/268638/en

    Vancouver: Copy

    Zareie Vahid, HAMIDZADEH MOGHADAM RASOUL. Interpretation of Magnetic Anomalies in Astmal Area using the Largest Eigenvalue. JOURNAL OF RESEARCH ON APPLIED GEOPHYSICS[Internet]. 2019;5(1 ):127-136. Available from: https://sid.ir/paper/268638/en

    IEEE: Copy

    Vahid Zareie, and RASOUL HAMIDZADEH MOGHADAM, “Interpretation of Magnetic Anomalies in Astmal Area using the Largest Eigenvalue,” JOURNAL OF RESEARCH ON APPLIED GEOPHYSICS, vol. 5, no. 1 , pp. 127–136, 2019, [Online]. Available: https://sid.ir/paper/268638/en

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