2009
DOI: 10.1016/j.ijrmms.2008.06.005
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Thermal stress in the Apuan marbles: Relationship between microstructure and petrophysical characteristics

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Cited by 54 publications
(27 citation statements)
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References 28 publications
(35 reference statements)
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“…The chemical composition of the powder reflects the mineralogical constituents of the different marble varieties. The grains are essentially composed by calcite (usually 95-99%), mainly in sand-to-silt sizes, with a small percentage (1-3%) of dolomite [15,22,23]. Silicates, primarily quartz, muscovite and/or chlorite and clay minerals, are often present in minor amounts [15,21].…”
Section: Chemical and Physical Features Of Marmettola And Karst Sprinmentioning
confidence: 99%
“…The chemical composition of the powder reflects the mineralogical constituents of the different marble varieties. The grains are essentially composed by calcite (usually 95-99%), mainly in sand-to-silt sizes, with a small percentage (1-3%) of dolomite [15,22,23]. Silicates, primarily quartz, muscovite and/or chlorite and clay minerals, are often present in minor amounts [15,21].…”
Section: Chemical and Physical Features Of Marmettola And Karst Sprinmentioning
confidence: 99%
“…Carrara marble was formed during the Apennine orogeny (Cantisani et al, ; Leiss & Molli, ). Lower to middle Liassic carbonate platform sequences were deformed and metamorphosed under greenschist facies conditions (Oesterling et al, ) and exposed in the Carrara nappe as a tectonic window (Leiss & Molli, ).…”
Section: Methodsmentioning
confidence: 99%
“…Other authors have shown that temperature variation is one of the main factors influencing the properties and physical integrity of stone materials. The thermal conductivity of the rocks is directly related to its consistency and, in general, increases with the decrease in porosity [13][14][15][16][17][18][19].…”
Section: Introductionmentioning
confidence: 99%