The results are presented for the investigations into the geological estimate of Macigno formation representing an Oligocene-Miocene turbiditic sequence of the Northern Apennines, from the coarse-graded beds of which the ldquoPietra Serenardquo quarry stone was mined. It is shown that the sedimentological features, the physico-mechanical properties, and the mineralogical composition of rocks govern the distinctions in the operating performances.

Pietra Serena mining in Fiesole: part II – geological setting of quarry / M. COLI; E. LIVI; E. PANDELI; C. TANINI. - In: JOURNAL OF MINING SCIENCE. - ISSN 1062-7391. - STAMPA. - 39:(2003), pp. 56-62.

Pietra Serena mining in Fiesole: part II – geological setting of quarry

COLI, MASSIMO;PANDELI, ENRICO;
2003

Abstract

The results are presented for the investigations into the geological estimate of Macigno formation representing an Oligocene-Miocene turbiditic sequence of the Northern Apennines, from the coarse-graded beds of which the ldquoPietra Serenardquo quarry stone was mined. It is shown that the sedimentological features, the physico-mechanical properties, and the mineralogical composition of rocks govern the distinctions in the operating performances.
2003
39
56
62
M. COLI; E. LIVI; E. PANDELI; C. TANINI
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Utilizza questo identificatore per citare o creare un link a questa risorsa: https://hdl.handle.net/2158/204420
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