Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin

Abstract Various karst processes and karst phenomena at scales from the macro to the micro occur in the cryolithozone of the middle Lena River basin. Karst processes have a warming impact on the enclosing perennially cryotic rocks and favour the formation of intra‐permafrost taliks at depths ranging...

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Published in:Permafrost and Periglacial Processes
Main Authors: Spektor, V. B., Spektor, V. V.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
lena river
permafrost
Permafrost and Periglacial Processes
Online Access:http://dx.doi.org/10.1002/ppp.639
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.639
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.639
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spelling crwiley:10.1002/ppp.639 2024-06-02T08:10:04+00:00 Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin Spektor, V. B. Spektor, V. V. 2009 http://dx.doi.org/10.1002/ppp.639 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.639 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.639 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 20, issue 1, page 71-78 ISSN 1045-6740 1099-1530 journal-article 2009 crwiley https://doi.org/10.1002/ppp.639 2024-05-06T07:01:56Z Abstract Various karst processes and karst phenomena at scales from the macro to the micro occur in the cryolithozone of the middle Lena River basin. Karst processes have a warming impact on the enclosing perennially cryotic rocks and favour the formation of intra‐permafrost taliks at depths ranging from a few to several tens of metres. Copyright © 2009 John Wiley & Sons, Ltd. Article in Journal/Newspaper lena river permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 20 1 71 78
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Various karst processes and karst phenomena at scales from the macro to the micro occur in the cryolithozone of the middle Lena River basin. Karst processes have a warming impact on the enclosing perennially cryotic rocks and favour the formation of intra‐permafrost taliks at depths ranging from a few to several tens of metres. Copyright © 2009 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Spektor, V. B.
Spektor, V. V.
spellingShingle Spektor, V. B.
Spektor, V. V.
Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin
author_facet Spektor, V. B.
Spektor, V. V.
author_sort Spektor, V. B.
title Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin
title_short Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin
title_full Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin
title_fullStr Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin
title_full_unstemmed Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin
title_sort karst processes and phenomena in the perennially frozen carbonate rocks of the middle lena river basin
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1002/ppp.639
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.639
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.639
genre lena river
permafrost
Permafrost and Periglacial Processes
genre_facet lena river
permafrost
Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 20, issue 1, page 71-78
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.639
container_title Permafrost and Periglacial Processes
container_volume 20
container_issue 1
container_start_page 71
op_container_end_page 78
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