Rare sulfides enriched in K, Tl and Pb from the Noril'sk and Salmagorsky complexes, Russia: new data and implications

摘要

New results (compositional data and reflectance values) are reported for some rare sulfides enriched in K, Tl and Pb, which are related to djerfisherite, thalfenisite, bartonite, a "Cl-bearing bartonite", or chlorbartonite, and also for shadlunite, from the Noril'sk and Salmagorsky complexes, Russia. Our observations and comparisons with relevant data in the literature imply that: (1) bartonite is probably a S-dominant (or Cl-free) analogue of djerfisherite; and a "Cl-bearing bartonite'' and chlorbartonite are probably compositional variants of the djerfisherite-bartonite series. (2) The most probable formulae of bartonite and djerfisherite are (K, Me2+)(6)(Fe, Cu, Ni)(25-x)S-26(S, Cl) and (K, Me2+)(6)(Fe, Cu, Ni)(25-x)S-26(Cl, S), where 0 <= x <= 5, respectively. (3) Two independent substitution mechanisms probably operate in the natural series. A coupled substitution [Me2+ + S2- <-> K+ + Cl-] is reflected by an observed deficit in K, accompanied by the incorporation of Me2+ (Pb, Fe, or Ni) in the K site. Another mechanism is inferred to be [2Fe(3+) + square <-> 3Fe(2+)], which assumes the existence of vacancy-type defects at the Me site. Thus, the second mechanism could possibly control the existing variations of Sigma(Fe, Cu, Ni) in the range of similar to 21 to 25 a.p.f.u., documented in djerfisherite-and bartonite-type minerals. The minerals analysed from Noril'sk, which are free of Cl and related to bartonite and to a Tl-dominant analogue of bartonite (unnamed species), probably crystallized from microvolumes of late fluid rich in K and Tl, under conditions of relatively low oxygen fugacity in the environment. Uniform contentss of Fe and Cu, observed in coexisting phases of normal (Cl-bearing) djerfisherite and bartonite (or Cl-free analogue of djerfisherite) at Salmagorsky imply that they reached equilibrium with regard to the distribution of these elements during crystallization. These phases probably formed as a result of fluctuations in the ratios of sulfur and chlorine fugacity in a fluid at a postmagmatic hydrothermal stage.