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A New approximate method for directly interpreting gravity anomaly profiles gaused by surfade geologic structures

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The problem of solving for the shape of a geologic body which exhibits a measured gravity anomaly has no direct solution in the general case.To obtain a satisfactory solution to such a problem with any degree of rigor,one must resort to a trial-and-error (iterative) solution.This problem is discussed for two-dimensional geometry in some detail by Bott(1960)and by Fournier and Krupicka (1973).An estimate of maximum depth to certain idealized bodies was suggested by Skeels (1963).

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Ketersediaan

Informasi Detail

Judul Seri

A NEW APPROXIMATE METHOD FOR DIRECTLY INTERPRETING GRAVITY ANOMALY PROFILES GAUSED BY SURFADE GEOLOGIC STRUCTURES

No. Panggil

PMB LU 1974 - 4 NL

Penerbit

Canada : by Surface geologic Structures., 1974

Deskripsi Fisik

Warna : Biru Halaman : 13

Bahasa

Indonesia

ISBN/ISSN

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Klasifikasi

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Tipe Isi

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Tipe Media

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Tipe Pembawa

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Edisi

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Subjek

laporan

Info Detail Spesifik

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Pernyataan Tanggungjawab

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Kode Wilayah

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Pulau Dan Lembar Peta

Lainnya

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Lainnya

Koordinat - Latitude

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Koordinat - Longitude

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