Interpretaçăo de Corpos Geológicos Magnetizados nas Baixas Latitudes - Corpos "Fantasmas

A.C. Motta

doi:10.3997/2214-4609-pdb.316.68

Interpretaçăo de Corpos Geológicos Magnetizados nas Baixas Latitudes - Corpos "Fantasmas
By A.C. Motta
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 2nd International Congress of the Brazilian Geophysical Society, Oct 1991, cp-316-00068
DOI: https://doi.org/10.3997/2214-4609-pdb.316.68

Abstract

O campo magnético da Terra, também chamado de campo geomagnético, provoca um campo secundário induzido antiparalelo em rochas que contęm minerais ferromagnéticos. A intensidade deste campo induzido é proporcional ŕ intensidade de campo geomagnético sendo a susceptibilidade magnética a constante de proporcionalidade de acordo com a fórmula: T* = kT, T* = campo induzido, T = campo geomagnético, K = susceptibilidade

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1991-10-28

2023-12-06

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Interpretaçăo de Corpos Geológicos Magnetizados nas Baixas Latitudes - Corpos "Fantasmas

Abstract

From This Site

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Most Cited This Month Most Cited RSS feed

The natural combination of full and image‐based waveform inversion

Poststack diffraction imaging using reverse‐time migration

Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture