Zobrazeno 1 - 10
of 264
pro vyhledávání: '"V G, Kuznetsov"'
Autor:
V. G. Kuznetsov, L. M. Zhuravleva
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 4, Pp 10-21 (2022)
Introduction. Until relatively recently, all carbonate rocks have been divided into organogenic and chemogenic rocks. The former group includes those half-composed of skeletal remains, thus representing a biological problem. The group of chemogenic c
Externí odkaz:
https://doaj.org/article/43e4b3fae52047ada033e7060a52a4ab
Autor:
V. G. Kuznetsov, L. M. Zhuravleva
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 3, Pp 8-18 (2022)
Introduction. Concepts describing bacterial effects on mineral formation and, first of all, on the formation of carbonate deposits, started to appear late in the 19th century both in Russia and globally. The precipitation of materials was demonstrate
Externí odkaz:
https://doaj.org/article/71d2a92ebda44a7394e70ef9d1893efb
Autor:
V. G. Kuznetsov
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 1, Iss 1, Pp 54-62 (2020)
This work analyses the development of reefs, which represent thick morphologically expressed carbonate massifs created by the activity of frame-forming organisms. Major stages in the development of reefs include the periods of Early Cambrian, Ordovic
Externí odkaz:
https://doaj.org/article/d29153a5fb114943a7e8d81d61d90c6e
Autor:
V. G. Kuznetsov, L. M. Zhuravleva
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 4, Pp 26-36 (2019)
There are five great cycles of reef formation in Paleozoic — Early Cambrian, Middle—Late Ordovician, Silu-rian—Devonian, Late Visean—Serpukhovian and Permian. Their upper limits are determined by the corresponding periods of biotic crises and
Externí odkaz:
https://doaj.org/article/db098b3147324b0da68d35d348689725
Publikováno v:
Литосфера, Vol 19, Iss 3, Pp 386-392 (2019)
Subject of research. The upper Permian reefs of the Yangtze block of southern China are considered. Among them there are two species which differ in location in the basin and the nature of the internal structure.Methods and results. On the basis of g
Externí odkaz:
https://doaj.org/article/20d22acf00904c1aa743eab98d891c66
Autor:
V. G. Kuznetsov
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 2, Pp 27-34 (2019)
The distribution in the geological section of two groups of sedimentary rocks, siliceous and carbonate rocks of different composition — has been examined. Acid-base conditions of external geospheres have been reconstructed in consideration of the p
Externí odkaz:
https://doaj.org/article/704ce8c36fa04f7aa7ae3f986eb46bfb
Autor:
V. G. Kuznetsov, A. N. Dmitrievsky
Publikováno v:
Lithology and Mineral Resources. 58:177-182
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5dfcb511d02a38616683c6e758d61dc1
https://doi.org/10.1134/s0024490222700018
https://doi.org/10.1134/s0024490222700018
Publikováno v:
Electrical engineering & Electromechanics, Iss 2, Pp 69-73 (2018)
Purpose. The resonant overvoltage arises in main electrical networks as a result of random coincidence of some parameters of circuit and its mode and it may exist for a relatively long time. Therefore, the traditional means of limitation of short dur
Externí odkaz:
https://doaj.org/article/017d8d198e08493294ea1caa6d0facef
Optical spectroscopy and unusual temperature shift of f – f zero-phonon luminescence lines: KTaO3:Er
Autor:
V. A. Trepakov, A. P. Skvortsov, Z. Potucek, Z. Bryknar, D. Nuzhnyy, V. Laguta, V. G. Kuznetsov, A. A. Gavrikov, A. Dejneka
Publikováno v:
Ferroelectrics. 591:191-200
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08a11bf05972eb41c26a708c4cc014d0
https://doi.org/10.1080/00150193.2022.2041938
https://doi.org/10.1080/00150193.2022.2041938
Autor:
V. G. Kuznetsov
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 3, Pp 27-30 (2016)
The informative and in the whole interesting and useful book of James Wilson and, in particular, a principal scheme of the standard facial zones are analyzed. The book is shown to reflect only one and not most important carbonate sedimentation enviro
Externí odkaz:
https://doaj.org/article/9e462e9f408c42f0b14cfecccdf45894