Типохимизм сульфидов Au-Pd-рудопроявления озерное (полярный Урал) in three associations (pyrrhotite-
pyrite, pyrrhotite-chalcopyrite-cubanite and bornite
Evolution of parental melts of alkali ultrabasic intrusive massives of Maimecha-Kotui Province (Polar Siberia) that the crystallization of olivine from the high-magnesium
pyrite melt occurred in the temperature range of 1510-1260 ° C
(Rare types of tetrahedrite-tennantite ores of a gold ore deposit.These sulphosalts occur as: 1) tiny segregations in sphalerite, galena and
pyrite; 2) thin veinlets
A genetic variety and convergence of epithermal gold-silver mineralization-molybdenum-porphyric and
pyrite ore assemblies as well as basic-ultrabasic complexes (gold-silver-telluride deposits), and also
Ultra dispersed magnetite as a catalyst for aquathermolysis of heavy oil derivative compounds of oxides such as maghemite,
pyrite and hematite. Besides the results of SARA
Up-dated ore composition data (Central ore-field, Kuznetsk Alatau)Bushmanov, A.,
Reva, I.,
Rudmin, M.,
Chernyshov, Aleksey I.,
Abramova, R.,
Voroshilov, V. was studied, as well as the distribution of trace elements in
pyrite.
Characteristic features of sulphide mineral DTA of
pyrite (550-580°) results in destruction of its superficial oxidized film. A thermal change typical