Zobrazeno 1 - 10
of 71
pro vyhledávání: '"Elena I. Demonterova"'
Autor:
Galina V. Pashkova, Mikhail A. Statkus, Maria M. Mukhamedova, Alexander L. Finkelshtein, Irina V. Abdrashitova, Olga Yu. Belozerova, Victor M. Chubarov, Alena A. Amosova, Artem S. Maltsev, Elena I. Demonterova, Dmitriy L. Shergin
Publikováno v:
Heritage, Vol 6, Iss 5, Pp 4434-4450 (2023)
In this study, the assessment of uncertainties introduced at different stages of the elemental analysis of archaeological ceramics has been described using the example of the Neolithic pottery sherds from Popovsky Lug (eastern Siberia). To evaluate t
Externí odkaz:
https://doaj.org/article/906baa7d48a342e9919bad5f8975b1b5
Autor:
Artem S. Maltsev, Nailya N. Umarova, Galina V. Pashkova, Maria M. Mukhamedova, Dmitriy L. Shergin, Vitaly V. Panchuk, Dmitry O. Kirsanov, Elena I. Demonterova
Publikováno v:
Molecules, Vol 28, Iss 3, p 1099 (2023)
The provenance study of archaeological materials is an important step in understanding the cultural and economic life of ancient human communities. One of the most popular approaches in provenance studies is to obtain the chemical composition of mate
Externí odkaz:
https://doaj.org/article/c1504fd24b0e43d190ac5edb23d2117a
Autor:
Anastasia V. Arzhannikova, Elena I. Demonterova, Marc Jolivet, Ekaterina A. Mikheeva, Alexei V. Ivanov, Sergey G. Arzhannikov, Valentin B. Khubanov, Vadim S. Kamenetsky
Publikováno v:
Geoscience Frontiers, Vol 13, Iss 1, Pp 101254- (2022)
The Late Paleozoic–Early Mesozoic Mongol-Okhotsk Ocean extended between the Siberian and Amur–North China continents. The timing and modalities of the oceanic closure are widely discussed. It is largely accepted that the ocean closed in a scissor
Externí odkaz:
https://doaj.org/article/723faef98af343bb8d5d3e6dcc143949
Publikováno v:
Minerals, Vol 11, Iss 4, p 357 (2021)
The Cheremkhovo formation (Pliensbachian) is the primary coal-bearing formation of the Irkutsk basin, Eastern Siberia. Still, few geochemical studies of the Jurassic sediments of the Irkutsk coal-bearing basin have been conducted, and there are no da
Externí odkaz:
https://doaj.org/article/54f1e8fd637748a8beb9e5a0a0a3447d
Autor:
Alexei V. Ivanov, Nikolay V. Vladykin, Elena I. Demonterova, Viktor A. Gorovoy, Emilia Yu. Dokuchits
Publikováno v:
Minerals, Vol 8, Iss 12, p 602 (2018)
The Malyy (Little) Murun massif of the Aldan Shield of the Siberian Craton has long been a kind of Siberian Mecca for geologists. It has attracted thousands of geologists, prospectors, and mineral collectors despite its remote location. It is famous
Externí odkaz:
https://doaj.org/article/3ca9e595e1ce42b9a506fa3d9c159353
Autor:
Anastasia V. Arzhannikova, Elena I. Demonterova, Alexander V. Sizov, Marc Jolivet, Ekaterina A. Mikheeva, Alexei V. Ivanov, Sergey G. Arzhannikov, Valentin B. Khubanov
Publikováno v:
International Geology Review
International Geology Review, In press, ⟨10.1080/00206814.2022.2139296⟩
International Geology Review, In press, ⟨10.1080/00206814.2022.2139296⟩
International audience; 12 The Early Cretaceous topographic evolution of Transbaikalia was largely governed by the 13 tectonic evolution of the Mongol-Okhotsk orogenic belt. The collapse of the Mongol-Okhotsk 14 orogen triggered the formation of meta
Publikováno v:
Russian Geology and Geophysics. 62:605-618
––A dike of rock similar in composition to carbonatites has been found in the Aikhal diamondiferous pipe of the Alakit–Markha field of the Yakutian kimberlite province (YaKP). The fine-grained rock of essentially carbonate composition (dolomite
Publikováno v:
Russian Geology and Geophysics. 62:291-305
—We performed a comprehensive study of basanites from the Daur–Hentiyn Range and present the first data on their Sr and Nd isotope and mineral compositions (electron probe microanalysis). The study has shown that the basanites are chemically simi
Publikováno v:
Geology of Ore Deposits. 63:54-78
—Metasomatic alterations in cataclased granites of the Primorsky Complex PR1 in the Southern Siberian Craton are represented by albitization and riebeckitization, accompanied by microclinization, dolomitization and completed by the formation of hyd
Autor:
Alexei V. Ivanov, Elena I. Demonterova, S.G. Arzhannikov, Ekaterina A. Mikheeva, Anastasia V. Arzhannikova, Marc Jolivet, V. B. Khubanov, Vadim S. Kamenetsky
Publikováno v:
Geoscience Frontiers
Geoscience Frontiers, Elsevier, 2022, 13 (1), pp.101254. ⟨10.1016/j.gsf.2021.101254⟩
Geoscience Frontiers, 2022, 13 (1), pp.101254. ⟨10.1016/j.gsf.2021.101254⟩
Geoscience Frontiers, Vol 13, Iss 1, Pp 101254-(2022)
Geoscience Frontiers, Elsevier, 2022, 13 (1), pp.101254. ⟨10.1016/j.gsf.2021.101254⟩
Geoscience Frontiers, 2022, 13 (1), pp.101254. ⟨10.1016/j.gsf.2021.101254⟩
Geoscience Frontiers, Vol 13, Iss 1, Pp 101254-(2022)
International audience; The Late Paleozoic–Early Mesozoic Mongol-Okhotsk Ocean extended between the Siberian and Amur–North China continents. The timing and modalities of the oceanic closure are widely discussed. It is largely accepted that the o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a749f5aba1ca22b10970027c5b7a2a09
https://hal-insu.archives-ouvertes.fr/insu-03266685/file/arzhannikova-2021.pdf
https://hal-insu.archives-ouvertes.fr/insu-03266685/file/arzhannikova-2021.pdf