UNIQUE ORE COMPLEXES IN THE NORTHWESTERN SECTOR OF THE PACIFIC ORE BELT
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Volkov A.V. | |
dc.contributor.author | Sidorov A.A. | |
dc.contributor.author | Tomson I.N. | |
dc.contributor.author | Savva N.E. | |
dc.date.accessioned | 2022-08-14T03:31:05Z | |
dc.date.available | 2022-08-14T03:31:05Z | |
dc.date.issued | 2004 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13469253 | |
dc.identifier.citation | Doklady Earth Sciences, 2004, 399, 9, 1185-1188 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38511 | |
dc.description.abstract | Using hierarchic ore-formation analysis methods it is shown that thin sulfidization zones in several regions represent the formations, whose composition most fully reflects mineralogical types of polychronous and monochronous ore-formation series (ore complexes). All members of the particular series possess certain indices of mutual mineralogical-geochemical relationship. It is shown that the large thin fluidization zones in terrestrial and volcanic-origin rock massifs have, apparently, different nature - from hydrothermal-sedimentary to epigenetic (plutonic-fluid). These, practically non-investigated zones, are the most important ore substance sources at porphyric and vein field formation. Together with many satellite deposits, including monochroous copper-, gold-, tin-porphyric series, they form unique ore complexes or polychronous ore-formation series. | |
dc.title | UNIQUE ORE COMPLEXES IN THE NORTHWESTERN SECTOR OF THE PACIFIC ORE BELT | |
dc.type | Статья |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru