На золоторудных проявлениях зеленокаменного пояса Кухмо (Восточная Финляндия) установлена устойчивая связь самородного золота и висмута (Йосиярви, Пиилола, Хеттеила), отражающих низкотемпературные условия образования в восстановительной обстановке. На рудопроявлениях Пиилола и Йосиярви золото-висмутовая минерализация ассоциирует с арсенопиритом, кристаллизация которого происходила при температуре 450-550°C. Золото совместно с висмутом кристаллизовалось в ретроградную фазу метаморфизма при температурах, соответствующих зеленосланцевой фации. Самородные золото и висмут, образующие включения в арсенопирите, можно интерпретировать как остаточный расплав. Преобладающее значение пирротина и магнетита (Хеттеила) в рудах, наряду с присутствием самородного висмута и мальдонита, свидетельствует о восстановительных условиях рудообразования и низкой фугитивности серы и теллура. Сделана попытка объяснения минералогических черт оруденения с позиций теории Liquid Bismuth Collector Model (LBCM). В качестве источника золота предполагаются рассеянные сульфиды вулканогенно-осадочного происхождения.
No abstract is provided for this article.
No abstract is provided for this article.
The article contains the results of statistical processing of geochemical data for rocks of the Porokhovskoe tungsten deposit (South Urals) obtained during systematic geological exploration. Statistical samplings were formed for various types of host rocks: andesites and their tuffs, shales, metasomatites (including sericite-quartz, epidote and chlorite-bearing) and skarns. It is established that all rocks of the Porokhovskoe deposit are characterized by increased contents of W and Mo and, to a lesser extent, Be, Cu, Li, and Zn and by stable groups of correlated elements, both associated with greisenization process and those inherited from the
 protolith. No zoning is revealed in the distribution of elements in relation to the Yugo-Konevsky leucogranitic pluton, which is considered the ore-generating for the deposit. No correlation between W and Mo was identifed in all types of host rocks. A number of statistical methods is proposed for the identifcation of promising areas with unclear W-Mo mineralization in rocks.
The review concerns the most interesting aspects of (mainly experimental) resonance tunnelling spectroscopy studies of a new type of heterosystems called van der Waals heterostructures. The possibility to compose such systems is a result of the recent discovery of two-dimensional crystals, a new class of materials derived from graphene. The role of the angular mismatch of the crystal lattices of conductive graphene electrodes in the tunnelling of charge carriers between them, as well as the closely related issues associated with fulfillment of the conservation laws during tunnelling transitions are considered. The experimental results on inelastic tunnelling in the graphene/h-BN/graphene heterosystems with strong angular mismatch are discussed. The experiments made it possible to determine the phonon density of states spectra of the constituent layers and to detect and describe tunnelling transitions involving localized states of structural defects in the h-BN barrier. We consider new results of studies on tunnelling and magnetotunnelling in van der Waals heterosystems that demonstrate the possibilities of practical application of resonant tunnelling effects in, e.g ., microwave engineering, based on realization of electronic devices having I – V curves with negative differential conductance (NDC) regions at tunnelling through defect levels of the barrier layers in such systems. These studies revealed two new types of heterosystems characterized by the formation of NDC regions as a result of resonant tunnelling through the defect levels in the h-BN barrier and by defect-assisted generation of tunnelling current. The bibliography includes 40 references.