NEW DATA ON HYDROCARBONS IN AURIFEROUS CONGLOMERATES OF THE WITWATERSRAND ORE REGION, REPUBLIC OF SOUTH AFRICA

dc.contributor.authorKremenetsky A.A.
dc.contributor.authorMaksimyuk I.E.
dc.date.accessioned2024-12-15T02:15:15Z
dc.date.available2024-12-15T02:15:15Z
dc.date.issued2006
dc.description.abstractGenesis of deposits in the world's largest Witwatersrand auriferous region (South Africa) remains a debatable issue over several decades. Based on geological and mineralogical-geochemical investigations, we previously proposed a sedimentary-exhalative hypothesis for its origin. In the present communication, we have attempted to develop and scrutinize this concept based on the study of organic matter in ore and nonore conglomerates, quartz in conglomerate pebbles, and fluid inclusions in quartz from pebbles and cement of ore and nonore conglomerates. © Pleiades Publishing, Inc., 2006.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13505984
dc.identifier.citationLithology and Mineral Resources, 2006, 41, 2, 102-116
dc.identifier.doi10.1134/S0024490206020027
dc.identifier.issn0024-4902
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46981
dc.titleNEW DATA ON HYDROCARBONS IN AURIFEROUS CONGLOMERATES OF THE WITWATERSRAND ORE REGION, REPUBLIC OF SOUTH AFRICA
dc.typeСтатья

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