2007
DOI: 10.1144/gsl.sp.2007.271.01.06
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Characterization of serpentinites to define their appropriate use as dimension stone

Abstract: Many questions arise when considering the appropriate use of building stones such as serpentinites. The commercial names of these rocks, collectively grouped as 'Green marbles', have no correspondence to their actual mineralogy, geochemistry and/or physical characteristics. Serpentinite being the hydrated product of an ultramafic parent rock and not a metamorphic product of limestone as implied by the term 'marble'. However, the serpentinites most widely used for ornamental purposes come from India (e.g. Rajas… Show more

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Cited by 25 publications
(22 citation statements)
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“…Correct identification and characterization of serpentine minerals is important in many fields such as the Earth and environmental sciences as well as the health sciences. For example, serpentinites (rocks composed dominantly of serpentine minerals) are commonly used for building materials and crushed aggregate . Chrysotile, characterized by rolled TO layers and a cylindrical/fibrous habit, was widely used as asbestos in insulating and fire‐resistant materials.…”
Section: Introductionmentioning
confidence: 99%
“…Correct identification and characterization of serpentine minerals is important in many fields such as the Earth and environmental sciences as well as the health sciences. For example, serpentinites (rocks composed dominantly of serpentine minerals) are commonly used for building materials and crushed aggregate . Chrysotile, characterized by rolled TO layers and a cylindrical/fibrous habit, was widely used as asbestos in insulating and fire‐resistant materials.…”
Section: Introductionmentioning
confidence: 99%
“…Approximately 5 % of Galicia (Spain) is covered by serpentinitic areas; these sites were formerly quarries from which materials for roads, ballast for railway, and ornamental rock were extracted (Pereira et al, 2007). The tailings left behind are often a source of contamination.…”
Section: Introductionmentioning
confidence: 99%
“…In the 0.10-0.20 m layer, soil Si contents did not fit any mathematical model, presenting a mean of 16.42 mg dm -3 ( Figure 1E). Pereira et al (2007) point out that Si presents low mobility in the soil, which may explain the higher levels in the layer where the serpentinite was added.…”
Section: Soil Chemical Attributesmentioning
confidence: 95%