Quartz sand resources in the Santa Maria Eterna formation, Bahia, Brazil: A geochemical and morphological study. (October 2015)

• Record Type: Journal Article
• Authors: Santos, Murilo Ferreira Marques dos; Fujiwara, Eric; Schenkel, Egont Alexandre; Enzweiler, Jacinta; Suzuki, Carlos Kenichi
• Is Part Of: Journal of South American earth sciences. Volume 62(2015:Oct.)
• Page Start: 176
• Page End: 185
• Publication Date: 2015-10
• Subjects: Quartz -- Trace elements in quartz -- Mineral resources -- Silica glass -- High purity quartz; Geology -- Latin America -- Periodicals; Earth sciences -- Latin America -- Periodicals; Geology -- Antarctica -- Periodicals; Earth sciences -- Antarctica -- Periodicals; Geology -- Caribbean Area -- Periodicals; Earth sciences -- Caribbean Area -- Periodicals; Géologie -- Amérique latine -- Périodiques; Sciences de la terre -- Amérique latine -- Périodiques; Géologie -- Antarctique -- Périodiques; Sciences de la terre -- Antarctique -- Périodiques; Géologie -- Caraïbes (Région) -- Périodiques; Sciences de la terre -- Caraïbes (Région) -- Périodiques; Earth sciences; Geology; Antarctica; Caribbean Area; Latin America; Periodicals; 550.5
• DOI: 10.1016/j.jsames.2015.06.002
• Languages: English
• ISSNs: 0895-9811

Abstract

Abstract: This study presents an evaluation of the quartz sand occurrences of the Santa Maria Eterna formation, in northeastern Brazil, as a potential source of raw material for silica glass manufacturing. Samples of quartz sand were analyzed by ICP-MS to determine a range of trace elements and establish its chemical purity. The technological potential of the sand was obtained by counting the quantity of bubbles formed during flame fusion over silica plate. Both chemistry and bubble formation indicate that the raw material is suitable for producing silica glass. The work also investigated the composition of fluid inclusions in the quartz grains and the surface micro-texture by scanning electron microscopy. With the results obtained by these procedures, we inferred that the quartz sand was probably formed in a marine environment, by the precipitation of silica in the form of quartz. The main impurities of the samples are probably present in the mineral inclusions implying that purification is possible and probably competitive. Highlights: This paper provides a geochemical analysis for a quartz sand deposit in Brazil. This work test the behavior of the quartz during fusion into silica glass. The tested deposit seems suitable for glass manufacturing. The geology and geochemistry indicates that the quartz was formed in a marine environment.