Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia
Abstract The formation of cement (pore) and intrusive ice in the frozen rocks of the central part of the Yakutian diamond‐bearing province is considered. Cement ice is best developed in the sedimentary rocks and kimberlite pipes. Intrusive ice is formed only in areas of considerable tectonic disturb...
Published in: | Permafrost and Periglacial Processes |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2002
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1002/ppp.408 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.408 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.408 |
id |
crwiley:10.1002/ppp.408 |
---|---|
record_format |
openpolar |
spelling |
crwiley:10.1002/ppp.408 2024-06-02T08:13:10+00:00 Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia Alexeev, Sergey V. Alexeeva, Ludmila P. 2002 http://dx.doi.org/10.1002/ppp.408 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.408 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.408 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 13, issue 1, page 53-59 ISSN 1045-6740 1099-1530 journal-article 2002 crwiley https://doi.org/10.1002/ppp.408 2024-05-03T11:05:19Z Abstract The formation of cement (pore) and intrusive ice in the frozen rocks of the central part of the Yakutian diamond‐bearing province is considered. Cement ice is best developed in the sedimentary rocks and kimberlite pipes. Intrusive ice is formed only in areas of considerable tectonic disturbance. The geochemistry of the ground ice is the result of cryogenic processes that cause salt differentiation during water freezing, together with natural solute concentration and cryogenic mineral formation. Copyright © 2002 John Wiley & Sons, Ltd. Article in Journal/Newspaper Permafrost and Periglacial Processes Yakutia Wiley Online Library Permafrost and Periglacial Processes 13 1 53 59 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Abstract The formation of cement (pore) and intrusive ice in the frozen rocks of the central part of the Yakutian diamond‐bearing province is considered. Cement ice is best developed in the sedimentary rocks and kimberlite pipes. Intrusive ice is formed only in areas of considerable tectonic disturbance. The geochemistry of the ground ice is the result of cryogenic processes that cause salt differentiation during water freezing, together with natural solute concentration and cryogenic mineral formation. Copyright © 2002 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Alexeev, Sergey V. Alexeeva, Ludmila P. |
spellingShingle |
Alexeev, Sergey V. Alexeeva, Ludmila P. Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia |
author_facet |
Alexeev, Sergey V. Alexeeva, Ludmila P. |
author_sort |
Alexeev, Sergey V. |
title |
Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia |
title_short |
Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia |
title_full |
Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia |
title_fullStr |
Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia |
title_full_unstemmed |
Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia |
title_sort |
ground ice in the sedimentary rocks and kimberlites of yakutia, russia |
publisher |
Wiley |
publishDate |
2002 |
url |
http://dx.doi.org/10.1002/ppp.408 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.408 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.408 |
genre |
Permafrost and Periglacial Processes Yakutia |
genre_facet |
Permafrost and Periglacial Processes Yakutia |
op_source |
Permafrost and Periglacial Processes volume 13, issue 1, page 53-59 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.408 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
13 |
container_issue |
1 |
container_start_page |
53 |
op_container_end_page |
59 |
_version_ |
1800736572936552448 |