By Vasco Fassina (Eds.)

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Because of its greater porosity, for both materials the inflection point in the initial part of the absorption curve is reached between 30 seconds and 5 minutes.

2. The peculiarity of the macroscopic markers (rust spots and balck xenoliths) is confirmed by X-ray diffraction patterns. 9. , 1829. Delrarchitettura di Marco Vitruvio Pollione libri dieci. , 1814. Viaggio ai Tre laghi, Maggiore, di Lugano e di Como, e ne' monti che li circondano. Milano. Anonymous, 1939. I marmi italiani. , 1853. I1 granito di Baveno. Milano. , 1948. Milano nell'arte e nella storia. , 1895. Principali cave di pietre da lavoro dell'alta Italia. Torino. , 1974. The Insubric and other tectonic lines in the Southern Alps.

The peculiarity of the macroscopic markers (rust spots and balck xenoliths) is confirmed by X-ray diffraction patterns. 9. , 1829. Delrarchitettura di Marco Vitruvio Pollione libri dieci. , 1814. Viaggio ai Tre laghi, Maggiore, di Lugano e di Como, e ne' monti che li circondano. Milano. Anonymous, 1939. I marmi italiani. , 1853. I1 granito di Baveno. Milano. , 1948. Milano nell'arte e nella storia. , 1895. Principali cave di pietre da lavoro dell'alta Italia. Torino. , 1974. The Insubric and other tectonic lines in the Southern Alps.

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