2019
DOI: 10.1140/epjp/i2019-12523-4
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Improvements to the analytical protocol of lapis lazuli provenance: First study on Myanmar rock samples

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Cited by 10 publications
(14 citation statements)
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“…Compositional data point analyses were collected using a SEM JEOL IT300LV equipped with an energy-dispersive X-ray spectrometer (EDX), with a SDD (a silicon drift detector from Oxford Instruments), hosted at the Earth Science Department of the University of Turin and already used for different applications (Vaggelli et al 2019).…”
Section: Scanning Electron Microscopementioning
confidence: 99%
“…Compositional data point analyses were collected using a SEM JEOL IT300LV equipped with an energy-dispersive X-ray spectrometer (EDX), with a SDD (a silicon drift detector from Oxford Instruments), hosted at the Earth Science Department of the University of Turin and already used for different applications (Vaggelli et al 2019).…”
Section: Scanning Electron Microscopementioning
confidence: 99%
“…Since ancient times, natural ultramarine has been obtained by grinding and purifying the semi-precious stone lapis lazuli (from the Latin lapis, stone, and lazalus, a latinized form of the Persian word for blue) [9]. Lapis lazuli is generically classified as a metamorphic rock, even if this definition could not be considered exhaustive, due to the complexity of mechanisms involved in its genesis [10]. Its blue colour is essentially due to the mineral called lazurite; in addition to lazurite, lapis lazuli is composed of several minerals whose presence and relative quantity varies according to the deposits of origin.…”
Section: Ultramarine and Azuritementioning
confidence: 99%
“…Petrographic analysis by optical microscope and SEM, together with the minero-chemical analysis of the main and accessory minerals by EDS microanalysis and the micro X-ray florescence determination of trace elements were used to characterise six samples representative of two historical quarries (Table 1). Petrographic analyses were carried out on polished thin sections, using a Cambridge S360 scanning electron microscope, according to the analytical conditions reported in [16]. In particular, the working distance was 25 mm; the probe current was 200 pA; the accelerating potential was 15 kV; the counting time resulted of 60 s. All the analyses were recalculated with MINSORT program by Petrakakis and Dietrich [17].…”
Section: Petrographic and Geochemical Characterisationmentioning
confidence: 99%