Paleomagnetism of the Siberian flood basalts of the Noril'sk area: A constraint on eruption duration

International Geology Review
By: , and 

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Abstract

The volcanic sequence of the Noril'sk area, northern Siberia, provides the most complete section of early Siberian flood-basalt volcanism. Paleomagnetic measurements for more than 4000 samples of lava and tuff indicate that nearly all of this >3500-m-thick sequence was laid down during one interval of normal magnetic polarity. Lavas of the lower third of this sequence are cut by the ore-bearing Noril'sk-I intrusion, which has an age of 251 Ma, identical to that of the Permian-Triassic boundary. Thus, the normal-polarity interval represented by this sequence is inferred to be the first of the Triassic Period. Eruption of this enormous volume of material in a relatively brief period coincident with the earth's greatest mass extinction requires that all aspects of Siberian flood-basalt volcanism be evaluated carefully as possibly contributing to that catastrophe.

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Publication type Article
Publication Subtype Journal Article
Title Paleomagnetism of the Siberian flood basalts of the Noril'sk area: A constraint on eruption duration
Series title International Geology Review
DOI 10.1080/00206819409465508
Volume 36
Issue 12
Year Published 1994
Language English
Publisher Taylor & Francis
Description 12 p.
First page 1139
Last page 1150
Country Russia
Other Geospatial Noril'sk Area, Siberia
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