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stibnite métalliques.
Stibnite, sometimes called antimonite, is a sulfide mineral with the formula Sb 2 S 3.This soft grey material crystallizes in an orthorhombic space group. It is the most important source for the metalloid antimony. The name is from the Greek στίβι stibi through the Latin stibium as the old name for the mineral and the element antimony.
This type of investigation was probably started by Drude (1888) when he obtained for stibnite such optical constants as the indices of refraction and coefficients of absorption, using a spectrometer equipped with rotatable nicols in the collimator and telescope tubes. ... GALOPIN, R., Différenciation chimique des mineraux métalliques par la ...
Le SOUFRE ÉLÉMENTAIRE et les SULFURES MÉTALLIQUES SOUES D’ÉNERGIE POUR DES MIROORGANISMES À la fin des années quarante, des chercheurs américains, Colmer et Hinkle, isolèrent des microorganismes (bactéries) qui avaient la popiété d’oxyder la pyrite (FeS 2) que contenaient les charbonnages de la Pennsylvanie (USA).
Stibnite is named after the latin stibium, which is the old name of the element antimony (Sb). Stibnite was and continues to be the primary ore of antimony. Stibnite forms some of the most outstanding natural crystals that exist, in way of sharpness, luster, and size.It can form in groups of huge metallic lustered crystals that are elegantly crafted and exceptionally shiny.
Stibnite is a very soft delicate mineral and should be kept in a container with a very soft cushion like cotton and not allowed to rub up against the sides of the box. Stibnite is a bit like graphite in that it will leave a streak when rubbed against paper. Over a period of many years, brilliant surfaces of freshly mined stibnite will become ...
Stibnite is the most abundant sulfide in both types of veins and appears to be the last sulfide in the paragenetic evolution. Consequently, it can be found in various textural positions. Two types of stibnite were distinguished: fine- to coarse-grained stibnite replacing berthierite (Fig. 5d) and stibnite
Late to post-Hercynian felsic intrusions can be divided in three groups (Cheilletz, 1984, Ntarmouchant, 1991): (1) an early calc-alkaline magmatic suite, composed of dikes of microgranodiorite, microgranite and rhyolite, with biotite granitic/granodioritic stocks, dated between 293.0 ± 3.0 and 287.9 ± 5.1 Ma; (2) late tholeiitic microdioritic and microtonalitic dikes; and (3) sparse ...
A fluid inclusion study in the polymetallic Brioude-Massiac district (French Massif Central) shows two main types of mineralizing fluids corresponding to two principal metallogenic cycles. The first cycle includes Sn−W−Au mineralizations as well as stibnite mineralization. These two types of parageneses originate from complex low saline and CO2-rich fluids and were deposited at rather high ...
Ayora Ibañez Carlos, Phillips Roy. Natural occurrences in the systems PbS — Bi 2 S 3 — Sb 2 S 3 and PbS — Sb 2 S 3 from Vall de Ribes, Eastern Pyrenees, Spain. In: Bulletin de Minéralogie, volume 104, 4, 1981. 12e assemblée générale de l'I.M.A. - Orléans – Juillet 1980.Deuxième partie : inclusions magmatiques / silicates / gemmes / « open session ».
This review summarizes the syntheses and applications of metal oxysulfides. Bulk compounds of rare earth and transition metals are discussed in the section Introduction. After a presentation of their main properties and applications, their structures are presented and their syntheses are discussed. The section Bulk Materials and Their Main Applications is dedicated to the growing field of ...
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Typical concentrations in unpolluted systems are less than 1 μg/l. The mean antimony concentration in surface marine waters is 184±45 ng/l (see Part I of this series, Filella et al., 2002a).Antimony concentrations are much higher in natural geothermal systems where they can range from 500 mg/l up to 10 wt.% Ritchie, 1961, Weissberg et al., 1979, Kolpakova, 1982, Stauffer and Thompson, 1984.
Stibnite and senarmontite have been identified by μRS and μXRD. Senarmontite can be observed as inclusions in stibnite ( Fig. 6 b) or as individual grains. Micro-Raman spectra show differences according to the orientation of the minerals with sharp bands at 45, 87, 143, 161, 183, 196, 216, 307, 473 cm −1 and a broader band centred at 707 cm ...
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