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THE INFLUENCE OF DIAGENETIC AND TECTONIC PROCESSES IN DOLOMITES ON THE GRINDING

Ivan Tomašić
Branko Salopek
Dragan Krasić


Puni tekst: hrvatski pdf 1.332 Kb

str. 47-51

preuzimanja: 901

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Sažetak

Origin and occurence of dolomites are important for the physical and mechanical properties, especially grinding. The influence of diagenetic and tectonic processes in dolomites on the grinding of rocks was investigated in samples from two diag-netically different deposit types, and that separately from the compact and tectonized part of the rock masses. The grinding tests were carried out in a ball mill. By petrographic and granulometric analysis as well as by determination of the grinding rate and Bond's Working Index it was found that the state of rock fissures influences the crushability down to grain sizes even of 1...2 mm, and that the grinding rate is lower for rocks of higher crystal lattice order and a higher content of small crystals. Also, samples with clean regular crystals, formed by recrystallization, manifest a stronger resistance to grinding.

Ključne riječi

Dolomites; Diagenetic and tectonic processes; Grinding

Hrčak ID:

24707

URI

https://hrcak.srce.hr/24707

Datum izdavanja:

4.12.1990.

Podaci na drugim jezicima: hrvatski

Posjeta: 2.021 *