2018116 · Many of the most extraordinary Namibian tourmalines come from two mines in particular which have acquired almost legendary status: Neu Schwaben and Usakos. Blue-green tourmaline from the Usakos mine. The cut stone weighs over twenty-eight carats and comes from the pocket discovered in 2016. Photo: Prangrak Ruahong.
view moreThe Canary mining area was originally worked for electronic-grade quartz (ca. 1982), and the brown tourmaline was tossed into the mine dumps (Njamu, 2003). Yellow tourmaline from eastern Zambia was first documented by Schmetzer and Bank (1983).
view more2023727 · Thermally modified tourmaline enhances hydrogen production by influencing hydrolysis acidification in two stages during dark fermentation of corn stover.
view more200021 · Abstract and Figures Silver-gray tourmaline fibers intergrown with a deep pink elbaite host from the Cruzeiro mine, Minas Gerais, Brazil, provide evidence for the compositional evolution of ...
view more202331 · Highlights • The formation of the Xianghualing tin deposit can be achieved by (1) fluid-rock interaction, and (2) late-stage magmatic volatile exsolution and cooling. • High oxygen fugacity or acid-consuming reactions are not necessary for cassiterite precipitation. • The evolution of sn-related magmatic-hydrothermal process based on …
view more2020112 · Coloured gemstones in eastern DRC: Tourmaline exploitation and trade in the Kivus Responsible sourcing efforts in the Democratic Republic of Congo (DRC) to date have focused predominantly on the so-called 3TG (tin, tungsten, tantalum and gold) sector. Nevertheless, the artisanal exploitation of other minerals including semi-precious …
view more202016 · the tourmaline-rich assemblages precipitated mostly from magmatic-hydrothermal fluids derived from their host plutons, mixed with minor external components sourced from metasedimentary, meta-ultramafic rocks, and/or meteoric water. The B-isotopic values increase sequentially from tourmaline patches to orbicules and/or cavities in both …
view more201861 · Like other deposits in the camp, the gold endowment at the Dome mine is the result of multistage, multi-process mineralization where main stage mineralization occurred towards the end of a period of deformation and magmatism ( Hutchinson, 1993, Goldfarb et al., 2001, Dubé and Gosselin, 2007, Washington, 2008, Washington et al., …
view moreJust Mining District. It is likely that these, and tourmaline-quartz ± rare cassiterite veins of similar orientation across southern Penwith, were formed in response to the same mineralization event. The Nanjizal schorl-cassiterite mineralization is similar to the quartz-tourmaline-cassiterite veins hosted by the Dartmoor Granite.
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