Zobrazeno 1 - 10
of 16
pro vyhledávání: '"L. V. Kuleshevich"'
Autor:
L. V. Kuleshevich, O. B. Lavrov
Publikováno v:
Geology of Ore Deposits. 64:123-143
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62a690ed74f8b8514a0877cce532f9b9
https://doi.org/10.1134/s1075701522030047
https://doi.org/10.1134/s1075701522030047
Autor:
L. V. Kuleshevich
Publikováno v:
Springer Proceedings in Earth and Environmental Sciences ISBN: 9783031233890
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4cc2fe322e9d1209663d707945cb103
https://doi.org/10.1007/978-3-031-23390-6_45
https://doi.org/10.1007/978-3-031-23390-6_45
Publikováno v:
Doklady Earth Sciences. 501:S7-S12
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cfc688b9981685233175fa692ad90065
https://doi.org/10.1134/s1028334x22010093
https://doi.org/10.1134/s1028334x22010093
Publikováno v:
Geochemistry International. 59:341-356
The paper presents results of the first geochronologic study (LA-ICP-MS zircon method) of metasedimentary rocks that host the banded iron formation (BIF) and the metarhyolites (halleflinta) of the Gimoly Group in the Kostimuksha greenstone belt,Karel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::853aa2fcacfe1a6a4ea80131df992dbc
https://doi.org/10.1134/s0016702921040066
https://doi.org/10.1134/s0016702921040066
Autor:
L. V. Kuleshevich
Publikováno v:
Vestnik of Geosciences. 9:14-18
Topomineralogical studies are part of mineralogenic research conducted in the Paleoproterozoic Lapland-Onega rift-related structure in Karelia. These studies are important because of the location of promising areas and the study of deposits associate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cee55406e2f4e1eb133e1e0751a7fad5
https://doi.org/10.19110/geov.2020.9.3
https://doi.org/10.19110/geov.2020.9.3
Autor:
A. V. Dmitrieva, L. V. Kuleshevich
Publikováno v:
Gornyi Zhurnal. :45-50
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ee0f16299e45283cd3f52bedf3ccc86
https://doi.org/10.17580/gzh.2019.03.09
https://doi.org/10.17580/gzh.2019.03.09
Publikováno v:
Литология и полезные ископаемые. :149-164
The Maksovo metasapropelite deposit, which contains shungite matter and is called maksovite, is located in the eastern Onega structure. The deposit is a diapiric fold which formed ca. 2070±10 Ma ago. It is underlain by carbonate rocks and overlain b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebc802a8eb44898c6833ac9854ca187f
https://doi.org/10.31857/s0024-497x20192149-164
https://doi.org/10.31857/s0024-497x20192149-164
Publikováno v:
Lithology and Mineral Resources. 54:145-158
The Maksovo shungite-bearing metasapropelite (maksovite) deposit is located in the eastern part of the Onega Basin that was initiated and formed in the Paleoproterozoic in the southeastern Fennoscandian Shield. The maksovite deposit represents a diap
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bfdb6ab141914beccf99650150aa7671
https://doi.org/10.1134/s0024490219020044
https://doi.org/10.1134/s0024490219020044
Autor:
O. B. Lavrov, L. V. Kuleshevich
Publikováno v:
Geology of Ore Deposits. 59:632-641
The Kaalamo massif is located in the Northern Ladoga region, Karelia, on the extension of the Kotalahti Belt of Ni-bearing ultramafic intrusions in Finland. The massif, 1.89 Ga in age, is differentiated from pyroxenite to diorite. Nickel–copper sul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c3327f810ca352260775cbb29295fc3e
https://doi.org/10.1134/s1075701517070066
https://doi.org/10.1134/s1075701517070066
Publikováno v:
Doklady Earth Sciences. 432:677-681
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f0b78d1e8eb4b0dae8bb56194dba4b70
https://doi.org/10.1134/s1028334x10050272
https://doi.org/10.1134/s1028334x10050272