CORRELATING VERTICAL MAGNETIC INTENSITY AND AVERAGE HORIZONTAL GRADIENTS OF GRAVlTY

Author:

Thyssen‐Bornemisza Stephen1

Affiliation:

1. Independent Geoscientist, New York, New York

Abstract

Average horizontal gradients of gravity observed with the gravity meter may communicate more information than a corresponding number of conventional Bouguer values if local conditions are favorable (Thyssen‐Bornemisza and Stackler, 1960, 1962; Thyssen‐Bornemisza, 1965). Several small experimental profiles of average horizontal gradients of gravity were taken over an area previously surveyed with the magnetometer, as shown in Figure 1.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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