Abstract

In order to determine the geologic boundaries such as contacts and faults, a high resolution technique has been developed in recent years, using the 2-order vertical derivative values of two horizontal gradients and one vertical gradient of the magnetic data. In this paper, the author constructed a program to interpret the magnetic data by using this method. This program can be applied easily for computation and the results can be presented under both types: maps and files. The program was illustrated in the interpretation of the magnetic data in a southernmost area of Viet-Num's Offshore.