Zobrazeno 1 - 7
of 7
pro vyhledávání: '"T. D. Karimov"'
Publikováno v:
Eurasian Soil Science. 54:551-559
A comparative study of modern flood sediments (floodplain alluvium) and sediments of the initial stage of overgrowing of oxbow lakes (oxbow alluvium) in the middle reaches of the Kamchatka River has been performed for the first time using group bioan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a9efc83ca539728f648f699fa6ecbd0
https://doi.org/10.1134/s1064229321040177
https://doi.org/10.1134/s1064229321040177
Autor:
S. B. Levchenko, V. Yu. Kuznetsov, Yu. V. Kushcheva, M. M. Pevzner, R. I. Nechushkin, A. Yu. Petrov, Fedor Maksimov, V. A. Grigor’ev, T. D. Karimov, O. N. Uspenskaya
Publikováno v:
Lithology and Mineral Resources. 56:71-88
A new reference section of the Okhotsk seaside of Kamchatka in the Mitoga 2 River area is studied and dated for the first time (14C and 230Th/U). Sedimentary deposits were correlated with the previously known sections in the Khomutina‒Mitoga interf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1dc4ed9ae8e9145ad267fdb10b80dbb8
https://doi.org/10.1134/s002449022006005x
https://doi.org/10.1134/s002449022006005x
Publikováno v:
Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 47, Iss 3, Pp 58-74 (2020)
The sediments of the floodplain of Kamchatka River in its middle course have been studied. Two types of floodplain accumulation environment are distinguished: stable (overgrowth of oxbow lakes distant from the main channel) and dynamic (banks of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::db3407b8e06170d0144c935dee4219b7
http://www.kscnet.ru/journal/kraesc/article/view/627
http://www.kscnet.ru/journal/kraesc/article/view/627
Autor:
N. A. Manucharova, A. L. Stepanov, A. P. Vlasova, N. A. Ksenofontova, T. D. Karimov, G. M. Zenova
Publikováno v:
Microbiology. 89:219-230
Molecular genetic techniques (FISH and metabarcoding) were used to investigate comparative biodiversity in the prokaryotic complex of soil microcosms of gray forest, chestnut, and chernozem soils before and after oil pollution. At the level of high-r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::509dd735d876d9fbda3b9b19c8f61e35
https://doi.org/10.1134/s0026261720020083
https://doi.org/10.1134/s0026261720020083
Publikováno v:
Литология и полезные ископаемые. :486-494
Radiocarbon studies of three pits in the upper Klyazma river basin near the village of Chashnikovo were carried out to determine the age of buried peat and soils. On the basis of nine radiocarbon dates, the age mark of the beginning of waterlogging o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6dcef89fd61a56ae1143eefaf7cf5a5
https://doi.org/10.31857/s0024-497x20195486-494
https://doi.org/10.31857/s0024-497x20195486-494
Autor:
O. Yu. Rozhdestvensky, M. M. Pevzner, O. I. Smyshlyaeva, R. I. Nechushkin, T. D. Karimov, O. V. Yashina
Publikováno v:
Lithology and Mineral Resources. 54:119-144
Reference sections of friable sediments in central Kamchatka are studied and their present-day state is described. Previous concepts of the Middle Pleistocene age of these sediments are critically examined. Radiocarbon dates performed in the 1980s‒
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d71b98f3fe1763ebebcfe1dcf2fa195
https://doi.org/10.1134/s0024490218060093
https://doi.org/10.1134/s0024490218060093
Autor:
M. M. Pevzner, O. V. Yashina, O. I. Smyshlyaeva, R. I. Nechushkin, T. D. Karimov, O. Yu. Rozhdestvensky
Publikováno v:
Литология и полезные ископаемые. 1:60-89
Reference sections of friable sediments in central Kamchatka are studied and their present-day state is described. Previous concepts of the Middle Pleistocene age of these sediments are critically examined. Radiocarbon dates performed in the 1980s‒
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2141efe5e8eed02774b83d59d3e53523
https://doi.org/10.31857/s0024-497x2019160-89
https://doi.org/10.31857/s0024-497x2019160-89