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Abstract

Geomagnetic studies integrated with geological ones at 1: 25 000 scale and smaller have helped the geological mapping, have determined the magmatic rocks below overlay, the dip angle of contacts between rocky types with magnetic distinctness and have outlined their tectonic structural features. They have also given opinions and solutions for the shape and continuity of ultrabasic and gabbroid massifs, etc. By analyzing and interpreting the character of the spreading of geomagnetic field anomaly is separated the zones in mineral-bearing of rocky types and in particularly the chromiferous of ultrabasic rocks. In sheet “75” (Vithkuqi) is carry out a complex geological-geophysical-geochemical study. Magnetometric survey has been carried out with the grid of (500x50) m, according to the lines of azimuth 650. Measurements of the intensity "T" and susceptibility "K" were carried out respectively by protonic magnetometer MP-2 (sensitivity ± 1nT) and capameter KT-5 (sensitivity 1x10-5 SI units).

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/content/papers/10.3997/2214-4609-pdb.262.R15
2011-10-03
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.262.R15
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