Secondary minerals in the geyserites of the Geysers Valley (Kamchatka)

Secondary minerals assemblages that are deposited from thermal solutions at the top of geysers (Velikan, Bolshoy) were investigated. It is established that assemblages are represented mainly by opal and high-silica zeolites (mordenite and heulandite). As conditions of feeding hydrothermal reservoir...

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Bibliographic Details
Published in:E3S Web of Conferences
Main Authors: Sergeeva Anastasia, Kiryukhin Alexey
Format: Article in Journal/Newspaper
Language:English
French
Published: EDP Sciences 2019
Subjects:
geo
envir
Kamchatka
Online Access:https://doi.org/10.1051/e3sconf/20199808019
https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_08019.pdf
https://doaj.org/article/c58720ea51ee4efc9670977f32e7eec1
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:c58720ea51ee4efc9670977f32e7eec1 2023-05-15T16:58:45+02:00 Secondary minerals in the geyserites of the Geysers Valley (Kamchatka) Sergeeva Anastasia Kiryukhin Alexey 2019-01-01 https://doi.org/10.1051/e3sconf/20199808019 https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_08019.pdf https://doaj.org/article/c58720ea51ee4efc9670977f32e7eec1 en fr eng fre EDP Sciences 2267-1242 doi:10.1051/e3sconf/20199808019 https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_08019.pdf https://doaj.org/article/c58720ea51ee4efc9670977f32e7eec1 undefined E3S Web of Conferences, Vol 98, p 08019 (2019) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.1051/e3sconf/20199808019 2023-01-22T18:03:48Z Secondary minerals assemblages that are deposited from thermal solutions at the top of geysers (Velikan, Bolshoy) were investigated. It is established that assemblages are represented mainly by opal and high-silica zeolites (mordenite and heulandite). As conditions of feeding hydrothermal reservoir change, minerals of the kaolinite group and smectites may appear. Article in Journal/Newspaper Kamchatka Unknown E3S Web of Conferences 98 08019
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
French
topic geo
envir
spellingShingle geo
envir
Sergeeva Anastasia
Kiryukhin Alexey
Secondary minerals in the geyserites of the Geysers Valley (Kamchatka)
topic_facet geo
envir
description Secondary minerals assemblages that are deposited from thermal solutions at the top of geysers (Velikan, Bolshoy) were investigated. It is established that assemblages are represented mainly by opal and high-silica zeolites (mordenite and heulandite). As conditions of feeding hydrothermal reservoir change, minerals of the kaolinite group and smectites may appear.
format Article in Journal/Newspaper
author Sergeeva Anastasia
Kiryukhin Alexey
author_facet Sergeeva Anastasia
Kiryukhin Alexey
author_sort Sergeeva Anastasia
title Secondary minerals in the geyserites of the Geysers Valley (Kamchatka)
title_short Secondary minerals in the geyserites of the Geysers Valley (Kamchatka)
title_full Secondary minerals in the geyserites of the Geysers Valley (Kamchatka)
title_fullStr Secondary minerals in the geyserites of the Geysers Valley (Kamchatka)
title_full_unstemmed Secondary minerals in the geyserites of the Geysers Valley (Kamchatka)
title_sort secondary minerals in the geyserites of the geysers valley (kamchatka)
publisher EDP Sciences
publishDate 2019
url https://doi.org/10.1051/e3sconf/20199808019
https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_08019.pdf
https://doaj.org/article/c58720ea51ee4efc9670977f32e7eec1
genre Kamchatka
genre_facet Kamchatka
op_source E3S Web of Conferences, Vol 98, p 08019 (2019)
op_relation 2267-1242
doi:10.1051/e3sconf/20199808019
https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_08019.pdf
https://doaj.org/article/c58720ea51ee4efc9670977f32e7eec1
op_rights undefined
op_doi https://doi.org/10.1051/e3sconf/20199808019
container_title E3S Web of Conferences
container_volume 98
container_start_page 08019
_version_ 1766050851879649280

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