THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA
The features of cyclic structure in the Karga-Sartan Ice Complex (IC) deposits in Northern Yakutia have been studied for the coastal lowlands. We have analyzed cycles of different genesis (cryolithological, structural, lithological, and soil-vegetation) and duration. Climate fluctuation was the majo...
Main Author: | |
---|---|
Format: | Article |
Language: | English |
Published: |
Lomonosov Moscow State University
2013-09-01
|
Series: | Geography, Environment, Sustainability |
Subjects: | |
Online Access: | https://ges.rgo.ru/jour/article/view/137 |
id |
doaj-b6576a90f24e49919f380ab63aec9e03 |
---|---|
record_format |
Article |
spelling |
doaj-b6576a90f24e49919f380ab63aec9e032021-07-28T21:10:05ZengLomonosov Moscow State UniversityGeography, Environment, Sustainability2071-93882542-15652013-09-016342010.24057/2071-9388-2013-6-3-4-20136THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIAVyacheslav KonishchevThe features of cyclic structure in the Karga-Sartan Ice Complex (IC) deposits in Northern Yakutia have been studied for the coastal lowlands. We have analyzed cycles of different genesis (cryolithological, structural, lithological, and soil-vegetation) and duration. Climate fluctuation was the major factor of cyclic structure in the IC deposits. Cyclic structure in the IC deposits develops in certain facial-genetic conditions characterized by cryogenic weathering and subsequent re-deposition of eroded soils in river valleys and alas depressionshttps://ges.rgo.ru/jour/article/view/137ice complexcyclicitycontentmineralogyweatheringsoilorigin |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Vyacheslav Konishchev |
spellingShingle |
Vyacheslav Konishchev THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA Geography, Environment, Sustainability ice complex cyclicity content mineralogy weathering soil origin |
author_facet |
Vyacheslav Konishchev |
author_sort |
Vyacheslav Konishchev |
title |
THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA |
title_short |
THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA |
title_full |
THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA |
title_fullStr |
THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA |
title_full_unstemmed |
THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA |
title_sort |
nature of cyclic structure of the ice complex, east siberia |
publisher |
Lomonosov Moscow State University |
series |
Geography, Environment, Sustainability |
issn |
2071-9388 2542-1565 |
publishDate |
2013-09-01 |
description |
The features of cyclic structure in the Karga-Sartan Ice Complex (IC) deposits in Northern Yakutia have been studied for the coastal lowlands. We have analyzed cycles of different genesis (cryolithological, structural, lithological, and soil-vegetation) and duration. Climate fluctuation was the major factor of cyclic structure in the IC deposits. Cyclic structure in the IC deposits develops in certain facial-genetic conditions characterized by cryogenic weathering and subsequent re-deposition of eroded soils in river valleys and alas depressions |
topic |
ice complex cyclicity content mineralogy weathering soil origin |
url |
https://ges.rgo.ru/jour/article/view/137 |
work_keys_str_mv |
AT vyacheslavkonishchev thenatureofcyclicstructureoftheicecomplexeastsiberia AT vyacheslavkonishchev natureofcyclicstructureoftheicecomplexeastsiberia |
_version_ |
1721262588463939584 |