ملخص
Investigates the use of Hilbert Transform in the analysis of magnetic anomalies caused due to a vertical fault. The first horizontal of the magnetic anomaly is transformed into vertical derivatives by means of Hilbert Transform. These 2 derivatives are made use of in the interpretation. The body parameters are obtained by means of simple and elegant mathematical expressions. Three theoretical examples are illustrated. A field example of total magnetic field pertaining to Lachlan foldbelt, New South Wales, Australia is incorporated. A brief discussion on the utility of amplitude, phase, envelope, and instantaneous frequency is also included. -Authors
اللغة الأصلية | English |
---|---|
الصفحات (من إلى) | 307-318 |
عدد الصفحات | 12 |
دورية | Acta Geodaetica, Geophysica et Montanistica Hungarica |
مستوى الصوت | 23 |
رقم الإصدار | 2-4 |
حالة النشر | Published - 1988 |
منشور خارجيًا | نعم |
ASJC Scopus subject areas
- ???subjectarea.asjc.2300.2300???
- ???subjectarea.asjc.1900.1900???