Boev, Blazo and Serafimovski, Todor (1996) Types of lateritic weathering crust along the Vardar river, Republic of Macedonia. Terranes of Serbia. pp. 427-432.
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Abstract
This paper is a brief account of the structural - metallogenic features of Ni-silicates and
Fe-Ni deposits in the Vardar zone along the Vardar
River volley in the Republic of Macedonia.
Two type of lateritic crusts were determined:
primary lateritic crusts - in situ (Groot, Gradiste
etc) and redeposited lateritic crusts (Rzanovo,
Siudena Voda, Rakle, Nikodin etc)
Litieritic crusts are genetically related to the
processes of lateritization of the Jurassic
serpentinites which took place in warm and wet
climate. They are basically nickeliferous -ferrugineous in which Ni content amounts to 1%, Fe to 32%, and Cr to about 2.5% co, V, Mn, Ti etc. occur as accompanying components.
Item Type: | Article |
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Uncontrolled Keywords: | weathering, lateritic crust, Vardar river, Macedonia |
Subjects: | Natural sciences > Other natural sciences |
Divisions: | Faculty of Natural and Technical Sciences |
Depositing User: | Blazo Boev |
Date Deposited: | 03 Dec 2012 14:42 |
Last Modified: | 10 Jun 2013 09:32 |
URI: | https://eprints.ugd.edu.mk/id/eprint/2948 |
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