Remote Sensing Analyses of Neotectonic Active Regions in East-Kamchatka

The tectonic history of the Kamchatka Peninsula is dominated by continuous accumulation and amalgamation of terranes with different origins, which were delivered by convergence between the Pacific plate and in former times, the Kula plate against Eurasia (Freitag, 2002). The Kronotsky and Cape Kamch...

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Main Authors: Jähne, Fabian, Freitag, Ralf
Format: Text
Language:German
Published: Universitätsverlag Göttingen 2006
Subjects:
Online Access:https://dx.doi.org/10.23689/fidgeo-1838
https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-3435-1
id ftdatacite:10.23689/fidgeo-1838
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spelling ftdatacite:10.23689/fidgeo-1838 2023-05-15T16:58:08+02:00 Remote Sensing Analyses of Neotectonic Active Regions in East-Kamchatka Jähne, Fabian Freitag, Ralf 2006 https://dx.doi.org/10.23689/fidgeo-1838 https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-3435-1 de ger Universitätsverlag Göttingen Text Article article-journal ScholarlyArticle 2006 ftdatacite https://doi.org/10.23689/fidgeo-1838 2021-11-05T12:55:41Z The tectonic history of the Kamchatka Peninsula is dominated by continuous accumulation and amalgamation of terranes with different origins, which were delivered by convergence between the Pacific plate and in former times, the Kula plate against Eurasia (Freitag, 2002). The Kronotsky and Cape Kamchatka Peninsulas show that the collision of terranes and the resulting tectonics are still important for major parts of East-Kamchatka. While the collision of the Kronotsky Peninsula is sorely influenced by the convergence of the Pacific plate, the Cape Kamchatka Peninsula is affected by the collision of the Aleutian Arc with Kamchatka, what gives the opportunity to compare two different processes that resulted in the amalgamation of terranes to Kamchatka. : conference Text Kamchatka Kamchatka Peninsula DataCite Metadata Store (German National Library of Science and Technology) Kamchatka Peninsula ENVELOPE(160.000,160.000,56.000,56.000) Pacific
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language German
description The tectonic history of the Kamchatka Peninsula is dominated by continuous accumulation and amalgamation of terranes with different origins, which were delivered by convergence between the Pacific plate and in former times, the Kula plate against Eurasia (Freitag, 2002). The Kronotsky and Cape Kamchatka Peninsulas show that the collision of terranes and the resulting tectonics are still important for major parts of East-Kamchatka. While the collision of the Kronotsky Peninsula is sorely influenced by the convergence of the Pacific plate, the Cape Kamchatka Peninsula is affected by the collision of the Aleutian Arc with Kamchatka, what gives the opportunity to compare two different processes that resulted in the amalgamation of terranes to Kamchatka. : conference
format Text
author Jähne, Fabian
Freitag, Ralf
spellingShingle Jähne, Fabian
Freitag, Ralf
Remote Sensing Analyses of Neotectonic Active Regions in East-Kamchatka
author_facet Jähne, Fabian
Freitag, Ralf
author_sort Jähne, Fabian
title Remote Sensing Analyses of Neotectonic Active Regions in East-Kamchatka
title_short Remote Sensing Analyses of Neotectonic Active Regions in East-Kamchatka
title_full Remote Sensing Analyses of Neotectonic Active Regions in East-Kamchatka
title_fullStr Remote Sensing Analyses of Neotectonic Active Regions in East-Kamchatka
title_full_unstemmed Remote Sensing Analyses of Neotectonic Active Regions in East-Kamchatka
title_sort remote sensing analyses of neotectonic active regions in east-kamchatka
publisher Universitätsverlag Göttingen
publishDate 2006
url https://dx.doi.org/10.23689/fidgeo-1838
https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-3435-1
long_lat ENVELOPE(160.000,160.000,56.000,56.000)
geographic Kamchatka Peninsula
Pacific
geographic_facet Kamchatka Peninsula
Pacific
genre Kamchatka
Kamchatka Peninsula
genre_facet Kamchatka
Kamchatka Peninsula
op_doi https://doi.org/10.23689/fidgeo-1838
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