MERCURY DISTRIBUTION IN TRAP ROCKS FROM THE SOUTHERN SIBERIAN PLATFORM

dc.contributor.author	Feoktistov G.D.
dc.date.accessioned	2021-02-25T05:13:21Z
dc.date.available	2021-02-25T05:13:21Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=13385830
dc.identifier.citation	Geochemistry International, 2001, 39, 2, 136-141
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/25707
dc.description.abstract	The study of mercury distribution in trap rocks from the southern Siberian Platform based on 260 determinations has shown that background Hg contents in trap sills pertaining to different intrusive phases are approximately equal (4.8 × 10-6 and 4.5 × 10-6 wt %) and close to the clarke value in the Earth's crust. Intrachamber fractionation does not affect mercury distribution. The hydrothermal alteration of trap rocks in iron-ore-bearing explosion pipes is accompanied by a partial removal of mercury.
dc.title	MERCURY DISTRIBUTION IN TRAP ROCKS FROM THE SOUTHERN SIBERIAN PLATFORM
dc.type	Статья

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