TRACE ELEMENT DISTRIBUTION IN THE KIMBERLITE-BITUMEN AND BASALT-BITUMEN SYSTEMS IN DIATREMES OF THE SIBERIAN CRATON

TRACE ELEMENT DISTRIBUTION IN THE KIMBERLITE-BITUMEN AND BASALT-BITUMEN SYSTEMS IN DIATREMES OF THE SIBERIAN CRATON

Gottikh R.P.; Pisotskii B.I.; Zhuravlev D.Z.
xmlui.dri2xhtml.METS-1.0.item-citation: Doklady Earth Sciences, 2004, 399, 9, 1222-1226
Date: 2004

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.

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