BIOGENIC MICROSTRUCTURES IN SHUNGITE ROCKS OF KARELIA
<p>The volcanosedimentary Zaonezhskaya Formation of the Ludicovian Suprahorizon (approximately 2.0 Ga) is well-known for grate hosting accumulation and a high content of carbonaceous matter. The rocks had been intruded by numerous mafic sills and later underwent lower greenschist-facies region...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Karelian Research Centre of the Russian Academy of Sciences
2017-02-01
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| Series: | Transactions of the Karelian Research Centre of the Russian Academy of Sciences |
| Subjects: | |
| Online Access: | http://journals.krc.karelia.ru/index.php/precambrian/article/view/318 |