Sedimentation rate as an indicator of the tectonic processes on the NW Black Sea shelf
Збережено в:
Дата: | 2015 |
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Автор: | |
Формат: | Стаття |
Мова: | English |
Опубліковано: |
2015
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Назва видання: | Geology and Mineral Resources of World Ocean |
Онлайн доступ: | http://jnas.nbuv.gov.ua/article/UJRN-0000882234 |
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Назва журналу: | Library portal of National Academy of Sciences of Ukraine | LibNAS |
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open-sciencenbuvgovua-675972024-04-16T13:29:57Z Sedimentation rate as an indicator of the tectonic processes on the NW Black Sea shelf M. V. Kozlenko 1999-7566 2015 en Geology and Mineral Resources of World Ocean http://jnas.nbuv.gov.ua/article/UJRN-0000882234 Article |
institution |
Library portal of National Academy of Sciences of Ukraine | LibNAS |
collection |
Open-Science |
language |
English |
series |
Geology and Mineral Resources of World Ocean |
spellingShingle |
Geology and Mineral Resources of World Ocean M. V. Kozlenko Sedimentation rate as an indicator of the tectonic processes on the NW Black Sea shelf |
format |
Article |
author |
M. V. Kozlenko |
author_facet |
M. V. Kozlenko |
author_sort |
M. V. Kozlenko |
title |
Sedimentation rate as an indicator of the tectonic processes on the NW Black Sea shelf |
title_short |
Sedimentation rate as an indicator of the tectonic processes on the NW Black Sea shelf |
title_full |
Sedimentation rate as an indicator of the tectonic processes on the NW Black Sea shelf |
title_fullStr |
Sedimentation rate as an indicator of the tectonic processes on the NW Black Sea shelf |
title_full_unstemmed |
Sedimentation rate as an indicator of the tectonic processes on the NW Black Sea shelf |
title_sort |
sedimentation rate as an indicator of the tectonic processes on the nw black sea shelf |
publishDate |
2015 |
url |
http://jnas.nbuv.gov.ua/article/UJRN-0000882234 |
work_keys_str_mv |
AT mvkozlenko sedimentationrateasanindicatorofthetectonicprocessesonthenwblackseashelf |
first_indexed |
2024-04-17T04:53:38Z |
last_indexed |
2024-04-17T04:53:38Z |
_version_ |
1796884329383591936 |