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Transformation peculiarities of gypsum cover of oil-Bearing strata in the outbreak zone (by example of Syukeyevskoye bitumen deposit)
Korolev E., Khuzin I., Galeev A., Ibragimov S.
appears due to inclusions of fine dispersed pyrite and magnetite, green-due to iron hydrosulfates. Pyrite
MAKALDER LEAD-ZINC PYRITE DEPOSIT (KENYA)
DZHASON S.O., DRUZHININ A.V., DOLGANEV V.P., KOVALENKER V.A.
MAKALDER LEAD-ZINC PYRITE DEPOSIT (KENYA)
Effect of the Natural Minerals Pyrite and Hematite on the Transformation of Domanik Rock Organic Matter in Hydrothermal Processes
Kayukova G., Mikhailova A., Kosachev I., Eskin A., Morozov V.
© 2019, Pleiades Publishing, Ltd. Abstract: The effect of the natural minerals pyrite and hematite
Efficiency increase for gold-bearing ore deposits with respect to the influence of sulfide surface nanobarrier on metal adsorption
Vorobyov A.E., Lyashenko V.I., Honore Tcharo, Vorobyev K.A.
with thereof type of gold in the form of pyrite and arsenopyrite disseminated mineralization is located
Transformation peculiarities of gypsum cover of oil-Bearing strata in the outbreak zone (by example of Syukeyevskoye bitumen deposit)
Korolev E., Khuzin I., Galeev A., Ibragimov S.
appears due to inclusions of fine dispersed pyrite and magnetite, green-due to iron hydrosulfates. Pyrite
COMPARATIVE ANALYSIS OF THE PROPERTIES OF NANORELIEF VARIOUS GOLD-BEARING SULPHIDES
Воробьев А.Е., Тчаро Х.
are presented. The morphology and microtopography of auriferous pyrite and arsenopyrite are described
СВЯЗЬ НАНОРЕЛЬЕФА ПИРИТА И АРСЕНОПИРИТА С ВЕЛИЧИНОЙ АДСОРБЦИИ ЗОЛОТА
Vorobev A.E., Kozyrev E.N., Тчаро Хоноре
are presented. The morphology and microtopography of gold-bearing pyrites and arse-nopyrites is described
EVALUATING RELATIONSHIP OF SELF-BURNING OF BREEDS WITH DEFORMATION PROCESSES IN THE COMBINED DEVELOPMENT OF SUMMARY ORE DEPOSITS
Rylnikova M.V., Radchenko D.N., Ainbinder G.I., Yesina E.N.
, prone to oxidation and spontaneous combustion. The mechanism of spontaneous combustion of pyritic rocks
Geochemical peculiarities of the Petropavlovsk gold deposit, Polar Ural [ГЕОХИМИЧЕСКИЕ ОСОБЕННОСТИ ПЕТРОПАВЛОВСКОГО ЗОЛОТОРУДНОГО МЕСТОРОЖДЕНИЯ (ПОЛЯРНЫЙ УРАЛ)]
Karelina E.V., Androsova N.K., Morozova T.P., Pavlinova N.V., Markov V.E.
. The principal metallic minerals are gold and pyrite; the latter is localized in the hydrothermally altered rocks
Accessory mineralization of dolomite reservoirs as the factor of fluids variability composition
Eskin A., Korolev E., Bakhtin A., Kolchugin A., Barieva E.
some iron accessory minerals such as siderite and pyrite. There are accessory crystals of quartz

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