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pro vyhledávání: '"V. D. Mats"'
Autor:
V. D. Mats
Publikováno v:
Геодинамика и тектонофизика, Vol 6, Iss 4, Pp 467-490 (2015)
The article reviews three typical concepts concerning the age of the Baikal rift (BR) which development is still underway: 5 Ma (the BR development start in the Late Pliocene), 30 Ma (Miocene or Oligocene), and 60–70 Ma (the Late Cretaceous). Under
Externí odkaz:
https://doaj.org/article/d20847f57c5a4aab8aa3e12028c86e94
Autor:
V. D. Mats
Publikováno v:
Stratigraphy and Geological Correlation. 21:637-651
The data obtained from long-term field studies in the Baikal Rift area are summarized. A new stratigraphic scheme is developed on the basis of previous stratigraphic research of N.A. Logachev. The new elements of the scheme are (1) the use of regiona
Publikováno v:
Stratigraphy and Geological Correlation. 19:404-423
Independent methods of geological and molecular-biological chronologies have made it possible to define generally corresponding stages in the geological and biological evolution of the environments and communities of Lake Baikal since the Late Cretac
Publikováno v:
Russian Geology and Geophysics. 51:650-660
This work is a review of the modern concepts of the accumulation of Fe and Mn in the Baikal bottom sediments and the regularities of formation of iron-manganese (including phosphate-bearing) nodules in the lake. Special attention is given to the prob
Publikováno v:
Stephan Mueller Special Publication Series. 2:161-170
Anomalies in pore water (PW) composition have been found in the 100 m-long core BDP-93 that was drilled in Southern Lake Baikal, in four piston cores taken from the same region, and in recent sediments from Frolikha Bay, a hydrothermal vent site in N
Publikováno v:
Scopus-Elsevier
New high-resolution seismic reflection data from the central part of Lake Baikal provide new insight into the structure and stratigraphy of Academician Ridge, a large intra-rift accommodation zone separating the Central and North Baikal basins. Four
Autor:
V. D. Mats, I. M. Yefimova
Publikováno v:
Geomorphology RAS. :67
The southwest end of Baikal rift is a slit-like gap incised into plateau - the relic of the Late Cretaceous-Paleogene (initial) peneplain. This is the most ancient element of the rift system. The plateau is transferred along-strike into Late Pliocene
Autor:
L. Z. Granina, S. S. Vorobyeva, Oleg Khlystov, E. L. Gol’dberg, M. A. Phedorin, M. Y. Semenov, V. D. Mats
Publikováno v:
Long Continental Records from Lake Baikal ISBN: 9784431679813
As a result of the limnological peculiarities of Lake Baikal, different forms of oxidized Fe and Mn accumulations are widely spread throughout the lake, not only in the uppermost sediments, but also within the sequence of reduced sediments. We presen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::147604af171491d4c42a0842691ee422
https://doi.org/10.1007/978-4-431-67859-5_13
https://doi.org/10.1007/978-4-431-67859-5_13
Publisher Summary This chapter discusses the interaction between the Lake Baikal water level and tectonism in the surrounding area, specially the Prebaikalye area. More specifically, the changing drainage process of Lake Baikal from the Lena River sy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f4857204f82b7c0b795d344e17ddfc08
https://doi.org/10.1016/b978-044450434-0/50003-2
https://doi.org/10.1016/b978-044450434-0/50003-2