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Economic Geology; August 1954; v. 49; no. 5; p. 451-492
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The ore deposits of Jugoslavia and the development of its mining industry

Friedrich Schumacher

The most important mineral deposits of Yugoslavia are nonferrous ores genetically related to Tertiary volcanic activity. They include the lead-zinc and antimony deposits of the Vardar tectonic trough, copper ores in the east Serbian block-faulted mountain belt, and numerous arsenic and molybdenum occurrences. Extensive chromite mineralization and smaller magnesite and asbestos deposits are associated with dislocated pre-Tertiry serpentine rocks mainly in south Serbia and adjacent parts of Macedonia. Hydrothermal iron ores and quicksilver-bearing tetrahedrite occurrences are among the mineral deposits associated with the Paleozoic limestone-schist complex of Bosnia. Sedimentary deposits include bedded and residual iron ores and widespread bauxite occurrences.

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JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
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