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GEOREF RECORD

The stones of medieval buildings in Pisa and Lucca (western Tuscany, Italy); 3, Green and white-pink quartzites from Mt. Pisano

Marco Franzini, Marco Lezzerini and Lorenzo Mannella
The stones of medieval buildings in Pisa and Lucca (western Tuscany, Italy); 3, Green and white-pink quartzites from Mt. Pisano
European Journal of Mineralogy (February 2001) 13 (1): 187-195

Abstract

The chemical, mineralogical, petrographic and main physical properties of 72 green and white-pink quartzite samples from Mt Pisano have been determined. They have a 'family' likeness and are mixtures in various proportions of silica and a 'residue'; the white-pink quartzites have an average quartz content of 71.60%, somewhat higher than the green ones (64.93%). Both types are extremely resistant to degradation. The white-pink (and green) quartzites have bulk density 2.44 (2.61) g/cm (super 3) , porosity 9.40 (3.39) vol.% and grain size 344 (175) mu m. The white-pink quartzites were much more frequently used in construction work, probably due to easier quarrying.


ISSN: 0935-1221
EISSN: 1617-4011
Serial Title: European Journal of Mineralogy
Serial Volume: 13
Serial Issue: 1
Title: The stones of medieval buildings in Pisa and Lucca (western Tuscany, Italy); 3, Green and white-pink quartzites from Mt. Pisano
Affiliation: Universita di Pisa, Dipartimento di Scienze della Terra, Pisa, Italy
Pages: 187-195
Published: 200102
Text Language: English
Publisher: Schweizerbart'sche Verlagsbuchhandlung (Naegele u. Obermiller), Stuttgart, Federal Republic of Germany
References: 17
Accession Number: 2001-022821
Categories: Igneous and metamorphic petrology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 5 tables, sketch maps
N43°45'00" - N43°45'00", E10°31'60" - E10°31'60"
Country of Publication: Germany
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United KingdomTwickenhamUKUnited Kingdom
Update Code: 200108
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