استفاده از تبدیل موجک بر روی داده های گرانی و تعیین عمق و شکل توده
Publish place: 12th Geophysics Conference of Iran
Publish Year: 1384
نوع سند: مقاله کنفرانسی
زبان: Persian
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شناسه ملی سند علمی:
GCI12_042
تاریخ نمایه سازی: 11 دی 1384
Abstract:
One of the main objectives in interpretation of gravimetric data is determination of depth and structure of the mineral deposits. This article tries to use the wavelet transform as a new method for achieving such a goal. The advantage of this technique over traditional methods is the ability of differentiating the small and large anomalies easily by using windows of different sizes. In this paper we try to apply this method on gravimetric data, to find the depth and structure of the mineral deposits and compare the results of an artificial model with hypothetical one. This method has proved to be satisfactory at least for the one dimensional example mentioned above.
Authors
حسین زمردیان
مدیر گروه ژئوفیزیک دانشگاه آزاد اسلامی واحد علوم و تحقیقات
بهنام بابایی
دانشجوی دوره دکترای پئوفیزییک اکتشاف دانشگاه آزاد اسلامی واحد علوم و ت