Zobrazeno 1 - 4
of 4
pro vyhledávání: '"S. N. Sedov"'
Autor:
A. V. Rusakov, S. N. Sedov
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 86, Pp 143-153 (2016)
The morphological record of pedogenesis (mostly at a micromorphological scale) and the features of paleosols developed at the northern geographical extremity of the MIS3 paleopedoshpere (including the Bryansk fossil soils) are described. The profiles
Externí odkaz:
https://doaj.org/article/5ae7e62bf2fa49a2ab8117195aaaaa40
Publikováno v:
Доклады Академии наук. 487:317-321
Rock freezing affects the soil complexes under maximal temperature gradients and forms a set of specific cryotrasological features in the solid soil matrix. When preserved these features serve as direct or indirect indicators of the past cryogenic co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e123e9d103b0f4167a6b1cb26d51a06f
https://doi.org/10.31857/s0869-56524873317-321
https://doi.org/10.31857/s0869-56524873317-321
Publikováno v:
Doklady Earth Sciences. 487:858-861
Rock freezing affects soil complexes with maximum temperature gradients and forms a set of the specific cryotrasologic features in a solid matrix of soils. Remaining unchanged, these features serve as direct and indirect indicators of the past cryoge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6255c3b6d214cc9fbee18bde707f9203
https://doi.org/10.1134/s1028334x19070274
https://doi.org/10.1134/s1028334x19070274
Publikováno v:
Doklady Earth Sciences. 2017. Vol. 477, part 2. P. 1430-1433
To solve the controversially debated problem related to the areal extent of the ice sheet in Western Siberia in the Quaternary period, we have studied the development of cold born objects of this area estimating the relationships between them in term
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::012614620bd1d23e8a71b3de89067890
https://doi.org/10.1134/s1028334x17120078
https://doi.org/10.1134/s1028334x17120078