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pro vyhledávání: '"Victor D. Mats"'
PALEOGEOGRAPHIC SCENARIO OF THE LATE CRETACEOUS – CENOZOIC FOR THE CENTRAL PART OF THE BAIKAL REGION
Autor:
Victor D. Mats, Irina M. Yefimova
Publikováno v:
Геодинамика и тектонофизика, Vol 2, Iss 2, Pp 175-193 (2015)
The publication presents a review of alterations of stagnant elements of the Baikal region that occurred during formation and development of the Baikal rift from the Late Cretaceous. Nowadays the natural complex contains the elements varying in age a
Externí odkaz:
https://doaj.org/article/f750e831a9d14a9482af37576f586333
タンデトロン加速器質量分析計業境報告 Summaries of Researches Using AMS 1994 (平成6)年度
Externí odkaz:
http://hdl.handle.net/2237/13276
Paleogeographic scenario of the Late Cretaceous - Cenozoic for the central part of the Baikal region
Autor:
Victor D. Mats, Irina M. Yefimova
Publikováno v:
Geodinamika i Tektonofizika, Vol 2, Iss 2, Pp 175-193 (2015)
The publication presents a review of alterations of stagnant elements of the Baikal region that occurred during formation and development of the Baikal rift from the Late Cretaceous. Nowadays the natural complex contains the elements varying in age a
Autor:
Victor D. Mats
Publikováno v:
International Geology Review. 58:1831-1832
This is a comment on the publication by Ivanov et al. (2015) on catastrophic outburst of Lake Baikal and provenance of the Palaeo-Manzurka sediments based on U-Pb dating of detrital zircons. The Paleo-Manzurka river system influenced largely the Baik
Publikováno v:
名古屋大学加速器質量分析計業績報告書. 6:161-166
タンデトロン加速器質量分析計業境報告 Summaries of Researches Using AMS 1994 (平成6)年度
Autor:
Victor D. Mats
Publikováno v:
Earth-Science Reviews. 34:81-118
The Baikal rift depression, located in southeastern Siberia, is one of the best investigated intra-continental rift structures in the world. In addition to being the site of comprehensive studies by Russian geo-scientists for decades, the Baikal depr
Autor:
Tatiana I. Perepelova, Victor D. Mats
Publikováno v:
Geoscience Frontiers, Vol 2, Iss 3, Pp 349-365 (2011)
A new model is suggested for the history of the Baikal Rift, in deviation from the classic two-stage evolution scenario, based on a synthesis of the available data from the Baikal Basin and revised correlation between tectonic–lithological–strati