ЗОНАЛЬНО-СЕКТОРИАЛЬНЫЕ КРИСТАЛЛЫ ПИРИТА-ВАЭСИТА ИЗ ГИДРОТЕРМАЛИТОВ В СЕРПЕНТИНИТАХ ЗАПАДНОГО АМАНБУЛАКА (ТУРКМЕНИЯ)
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dc.contributor.author | Попов В.А. | |
dc.contributor.author | Попова В.И. | |
dc.contributor.author | Власова И.В. | |
dc.contributor.author | Недосекова И.Л. | |
dc.contributor.author | Нишанбаев Т.П. | |
dc.date.accessioned | 2024-04-06T00:47:26Z | |
dc.date.available | 2024-04-06T00:47:26Z | |
dc.date.issued | 2006 | |
dc.identifier | https://elibrary.ru/item.asp?id=9438967 | |
dc.identifier.citation | Записки Российского минералогического общества, 2006, 135, 6, 38-41 | |
dc.identifier.issn | 0869-6055 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/43388 | |
dc.description.abstract | There are characterized compositions of pyrite, millerite, bravoitc, vaesite, gcrsdorfite, polydymite and sphalerite. Zonal-sectorial crystals of pyrite-vaesite have overgrown upon needle-shaped millerite. Octahedral zones of the pyritc-vaesite crystals are composed only of vaesite (51 %al Ni), whereas their cube zones - of vaesite and pyrite (4 %„, Ni) rhythmically alternate with each other. Subsequently those crystals were overgrown by oriented gersdorfite. | |
dc.title | ЗОНАЛЬНО-СЕКТОРИАЛЬНЫЕ КРИСТАЛЛЫ ПИРИТА-ВАЭСИТА ИЗ ГИДРОТЕРМАЛИТОВ В СЕРПЕНТИНИТАХ ЗАПАДНОГО АМАНБУЛАКА (ТУРКМЕНИЯ) | |
dc.type | Статья | |
dc.subject.udc | 549.324.3 |
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