NDLI: Zones of activation and volcanism

Content Provider	Springer Nature Link
Author	Sidorov, A. A. Volkov, A. V. Alekseev, V. Yu.
Copyright Year	2013
Abstract	The zones of tectono-magmatic activation (TMA) that bound and traverse the major volcanogenic belts in the Russian Northeast were previously thought to be satellites of these belts. We even suggested an appropriate term, “perivolcanic zones” [Sidorov et al., 1978]. However, these supra-subduction and their perivolcanic zones are generally radically different from the deep-seated TMA zones of the Chukchi or Omsukchan types in that they are less deep and are short-lived. In contrast to volcanogenic belts, which are characterized by numerous small volcanic features with numerous mineralization occurrences of base and noble metals among regional propilitization fields, it is exactly in the zones of activation of these types that long-lived, volcano-plutonic centers with major mineralization fields are formed.
Starting Page	185
Ending Page	195
Page Count	11
File Format	PDF
ISSN	07420463
Journal	Journal of Volcanology and Seismology
Volume Number	7
Issue Number	3
e-ISSN	18197108
Language	English
Publisher	Springer US
Publisher Date	2013-07-07
Publisher Place	Boston
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Geophysics/Geodesy Geochemistry Geology
Content Type	Text
Resource Type	Article
Subject	Geology Geochemistry and Petrology Geophysics

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Zones of activation and volcanism