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                <identifier>ezaposleni.singidunum.ac.rs/rest/sciNaucniRezultati/oai:1:6968</identifier>
                <datestamp>2019-05-28T06:38:42Z</datestamp>
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                    <dim:field mdschema="dc" element="title" lang="en">ORE MINERALIZATION AT STUDIED GEOMAGNETIC ANOMALIES ON MT. GOLIJA</dim:field>
                    <dim:field mdschema="dc" element="date" qualifier="issued">2016</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="uri">http://ezaposleni.singidunum.ac.rs/rest/sciNaucniRezultati/oai/record/1/6968</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="uri">http://eprints.ugd.edu.mk/16342/7/GeolCongr%202016%20The%20Vrshnik%20Filev.pdf</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:27031" confidence="-1">J. Kovačević</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="etfid:888" confidence="-1">B. Vakanjac</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:27033" confidence="-1">D. Nikolić</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:27034" confidence="-1">M. Pandurov</dim:field>
                    <dim:field mdschema="dc" element="description" qualifier="abstract">The geologic framework, tectonic assemblage, magmatism and rock alterations of Mt. Golija are such that it is
predisposed to deposits of non-ferrous metals, iron, tungsten and other metallic and non-metallic minerals. The
objective of the research reported in this paper was to identify aeromagnetic anomalies and undertake
prospecting investigations in selected areas, in search of any previously unknown or undetected occurrences of
metallic mineral ores. Already known ore-bearing areas were also expected to expand if occurrences were
detected in only one part of the selected study area or were solitary within that area. Without doubt, Tertiary
igneous rocks have basically caused the anomalous field on Mt. Golija. Skarn ore with magnetite was also a
likely contributor, but to a lesser extent. The involvement of volcanites was expected to be somewhat more
pronounced through the influence of covered, younger sub-volcanic intrusions. There was an evident effect of
volcanites, with a reversed magnetic field, which was manifested by an individualized negative anomaly at
Muhovo. Most of the samples were collected at the following localities: Tikveš – Truba, Ostatija – Biser Voda
and Radulovac – Kolesnička River. Ore mineralizations in the study area were found to be diverse by type,
transformation and alteration of detected minerals. In effect, sampling was undertaken to verify the recorded
anomalies. The present paper discusses testing of ore mineralization in the area where magnetic anomalies had
been detected.</dim:field>
                    <dim:field mdschema="dc" element="type">conferenceObject</dim:field>
                    <dim:field mdschema="dc" element="citation" qualifier="spage">559</dim:field>
                    <dim:field mdschema="dc" element="citation" qualifier="epage">568</dim:field>
                    <dim:field mdschema="dc" element="source">Трет Конгрес на Геолозите на Република Македонија Зборник на трудови Книга 2</dim:field>
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