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  1. Journal of Volcanology and Seismology
  2. Journal of Volcanology and Seismology : Volume 9
  3. Journal of Volcanology and Seismology : Volume 9, Issue 6, November 2015
  4. Volcanism and epithermal deposits
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Journal of Volcanology and Seismology : Volume 11
Journal of Volcanology and Seismology : Volume 10
Journal of Volcanology and Seismology : Volume 9
Journal of Volcanology and Seismology : Volume 9, Issue 6, November 2015
Volcanism and epithermal deposits
The geochemistry of manganese conglomerates on the Vityaz’ Rise, Japan Sea
Thermal anomalies on Savich Cone, Kikhpinych Volcano, Kamchatka: IR surveys and land-based observations for 30 years (1982 through 2012)
A study of the focal mechanisms of small volcanic earthquakes during the precursory period and the occurrence of the 2008–2009 eruption on Koryakskii Volcano
Correlative relationships between tsunami height and strong ground motion parameters: Japanese earthquakes
The Urup earthquake sequence of 2012–2013
Analysis of the unusual earthquake of 13 August 2006 in Michoacán, México
Journal of Volcanology and Seismology : Volume 9, Issue 5, September 2015
Journal of Volcanology and Seismology : Volume 9, Issue 4, July 2015
Journal of Volcanology and Seismology : Volume 9, Issue 3, May 2015
Journal of Volcanology and Seismology : Volume 9, Issue 2, March 2015
Journal of Volcanology and Seismology : Volume 9, Issue 1, January 2015
Journal of Volcanology and Seismology : Volume 8
Journal of Volcanology and Seismology : Volume 7
Journal of Volcanology and Seismology : Volume 6
Journal of Volcanology and Seismology : Volume 5
Journal of Volcanology and Seismology : Volume 4
Journal of Volcanology and Seismology : Volume 3
Journal of Volcanology and Seismology : Volume 2
Journal of Volcanology and Seismology : Volume 1

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Volcanism and epithermal deposits

Content Provider Springer Nature Link
Author Sidorov, A. A. Volkov, A. V. Savva, N. E.
Copyright Year 2015
Abstract Epithermal mineralization is an important metallogenic criterion for volcanogenic belts of varying ages. We show that epithermal high-sulfidation deposits are shallow formations in volcanogenic belts, with low-sulfidation deposits being formed at the subvolcanic level and the intermediate between the two types being the deepest deposits. Regenerated deposits make up their own group. Deposits of each type have been characterized. Typical epithermal deposits had been formed before a granitoid plutonic source came into being. The abundance of quartz–chalcedony amygdules in basaltoids that are found in several ore areas can be explained by their temporal connections to hydrothermal systems that stopped functioning during and after the emplacement of basaltic magmas. It is hypothesized that the concentration of post-mineralization basaltoid dikes within ore fields of epithermal deposits was due to the activity of a “microplume,” which was the cause of late (rhyolite and granitoid) magmatism, hydrothermal activity, and epithermal mineralization.
Starting Page 349
Ending Page 357
Page Count 9
File Format PDF
ISSN 07420463
Journal Journal of Volcanology and Seismology
Volume Number 9
Issue Number 6
e-ISSN 18197108
Language English
Publisher Pleiades Publishing
Publisher Date 2015-12-24
Publisher Place Moscow
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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