ТЕХНОГЕННЫЕ СУЛЬФАТЫ ОЛОВОСУЛЬФИДНЫХ МЕСТОРОЖДЕНИЙ ДАЛЬНЕГО ВОСТОКА

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dc.contributor.author Зверева В.П.
dc.contributor.author Афанасьева Т.Б.
dc.contributor.author Баринов Н.Н.
dc.contributor.author Нарнов Г.А.
dc.contributor.author Бахарева Г.А.
dc.date.accessioned 2022-12-03T09:10:07Z
dc.date.available 2022-12-03T09:10:07Z
dc.date.issued 2005
dc.identifier https://www.elibrary.ru/item.asp?id=9142820
dc.identifier.citation Записки Российского минералогического общества, 2005, 134, 4, 83-86
dc.identifier.issn 0869-6055
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/40714
dc.description.abstract Long-term functioning of mining industry in the region has given rise to development of technogenic sys-tems, in which hypergene processes provide crystallization of secondary polymineral formations. They are repre-sented as crusts (up to 50 cm in thickness), sinters, incrustations, veinlets and stalactite-stalagmite forms develo-ped over waste dumps, tailings, on walls and timbering of mining workings, in host rock, etc. Study of this newly formed mineral substances by roentgenostructural, electron-microscopic, IR-spectroscopic methods and chemi-cal analyses has detected among them chalcanthite, alunogen, siderotil, pickeringite, halotrichite, starkeyite, diet-richite, and some other minerals.
dc.title ТЕХНОГЕННЫЕ СУЛЬФАТЫ ОЛОВОСУЛЬФИДНЫХ МЕСТОРОЖДЕНИЙ ДАЛЬНЕГО ВОСТОКА
dc.type Статья
dc.subject.udc 504.054:553.45(571.6)


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