TRACE ELEMENT DISTRIBUTION IN THE KIMBERLITE-BITUMEN AND BASALT-BITUMEN SYSTEMS IN DIATREMES OF THE SIBERIAN CRATON
| dc.contributor.author | Gottikh R.P. | |
| dc.contributor.author | Pisotskii B.I. | |
| dc.contributor.author | Zhuravlev D.Z. | |
| dc.date.accessioned | 2022-07-20T06:12:22Z | |
| dc.date.available | 2022-07-20T06:12:22Z | |
| dc.date.issued | 2004 | |
| dc.description.abstract | The present paper considers trace element distribution in two natural systems: kimberlite-bitumen and basalt-bitumen. In the given case, carbonaceous matter in magmatic rocks is interpreted as a result of abiogenic synthesis from fluid components of melts at the final magmatic (pneumatolytic-hydrothermal) stages. | |
| dc.identifier | https://www.elibrary.ru/item.asp?id=13458839 | |
| dc.identifier.citation | Doklady Earth Sciences, 2004, 399, 9, 1222-1226 | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38323 | |
| dc.title | TRACE ELEMENT DISTRIBUTION IN THE KIMBERLITE-BITUMEN AND BASALT-BITUMEN SYSTEMS IN DIATREMES OF THE SIBERIAN CRATON | |
| dc.type | Статья |