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К проблеме петрогенезиса карбонат-тальковой толщи Кривбасса
New evidence of the stratified volcanogenic nature of metaultrabasites of the talcous subsuit of the Early Pre-Cambrian Kryvorizhsky metamorphic series has been obtained. A group of sedimentary volcanicterrigenous rocks (metaaleuropelites) synchronous and closely connected with ultrabasic volcanicit...
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| Main Authors: | , |
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| Format: | Article |
| Language: | Russian |
| Published: |
Видавничий дім "Академперіодика" НАН України
2008
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| Subjects: | |
| Online Access: | http://dspace.nbuv.gov.ua/handle/123456789/3906 |
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| Summary: | New evidence of the stratified volcanogenic nature of metaultrabasites of the talcous subsuit of the Early Pre-Cambrian Kryvorizhsky metamorphic series has been obtained. A group of sedimentary volcanicterrigenous rocks (metaaleuropelites) synchronous and closely connected with ultrabasic volcanicity are petrochemically diagnosed. By a degree of enrichment of these meta-aleuropelites with Fe, Mg, Ca, Cr components, they form a progressive series from ordinary low-ferrousmagnesia aluminiferous phyllite of the Skelevatskaya suite to anomalous highferrous-magnesia differences enriched with calcium and chromium approaching ultrabasites of the talcous horizon to a greater or lesser extent. |
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