ملخص
A simple method to interpret gravity gradients over a thin infinite dipping sheet is discussed. The Hilbert transform is used to compute the vertical gradient from the horizontal gradient of the gravity field. The method is illustrated with a theoretical example.
اللغة الأصلية | English |
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الصفحات (من إلى) | 11-14 |
عدد الصفحات | 4 |
دورية | Proceedings of the Indian Academy of Sciences - Earth and Planetary Sciences |
مستوى الصوت | 96 |
رقم الإصدار | 1 |
حالة النشر | Published - مارس 1987 |
منشور خارجيًا | نعم |
ASJC Scopus subject areas
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