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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