Zobrazeno 1 - 8
of 8
pro vyhledávání: '"L. V. Eirish"'
Autor:
A. Yu. Kadashnikova, V. A. Ponomarchuk, L. V. Eirish, A. A. Sorokin, A. I. Dementienko, A.V. Ponomarchuk, A. V. Travin
Publikováno v:
Russian Journal of Pacific Geology. 13:575-584
The paper reports the results of 40Ar/39Ar geochronological studies of the muscovite–quartz–albite metasomatites of the ore bodies and host rocks of the Albyn deposit located in the Selemdzha–Kerbi structural zone of the eastern part of the Mon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8df770cd4b1e029c1128e0343dc65a4e
https://doi.org/10.1134/s1819714019060046
https://doi.org/10.1134/s1819714019060046
Autor:
A. Yu. Kadashnikova, А. V. Travin, A.V. Ponomarchuk, А. А. Sorokin, V. А. Ponomarchuk, L. V. Eirish, A. I. Dementienko
Publikováno v:
Доклады Академии наук. 485:468-473
It was established that the age of hydrothermal metasomatites of the Albyn gold deposit, one of the most famous in eastern Asia, can be estimated at 135-131 Ma. It is assumed that the formation of this deposit is associated with dislocations and meta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::35b6803e03a57e4c625587e992888526
https://doi.org/10.31857/s0869-56524854468-473
https://doi.org/10.31857/s0869-56524854468-473
Autor:
A. A. Kadashnikova, A. A. Sorokin, A. V. Ponomarchuk, A. V. Travin, V. A. Ponomarchuk, A. I. Dementienko, L. V. Eirish
Publikováno v:
Doklady Earth Sciences. 485:358-362
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14169ea799bb2c6a11cabda6bc326ee0
https://doi.org/10.1134/s1028334x19040056
https://doi.org/10.1134/s1028334x19040056
Autor:
A.V. Ponomarchuk, L. V. Eirish, A. V. Travin, A. Yu. Kadashnikova, A. A. Sorokin, V. A. Ponomarchuk
Publikováno v:
Geology of Ore Deposits. 61:1-13
A reliable estimate is obtained for the gold mineralization age for the Malomyr deposit (eastern part of the Mongol–Okhotsk Fold Belt), one of the most well-known in the Russian Far East. The obtained data indicate that the age of the hydrothermal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bfc027bab921d4436da00074824d3d4d
https://doi.org/10.1134/s1075701519010045
https://doi.org/10.1134/s1075701519010045
Autor:
L. V. Eirish
Publikováno v:
Russian Journal of Pacific Geology. 5:85-88
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebd3193a0bf8104ce0826c6790df24e4
https://doi.org/10.1134/s1819714011010039
https://doi.org/10.1134/s1819714011010039
Autor:
L. V. Eirish
Publikováno v:
Geology of Ore Deposits. 51:223-232
Relationships of gold mineralization to deep-seated low-density domains of granitization are considered. The gold mineralization originates in the zones of interaction of these domains with femic rocks established from the results of regional magneti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43e0dd67c87a2b3f8135865ea79157ff
https://doi.org/10.1134/s1075701509030040
https://doi.org/10.1134/s1075701509030040
Autor:
L. V. Eirish
Publikováno v:
Russian Journal of Pacific Geology. 2:454-463
The intensity of placer formation is controlled by many factors, mainly by the erosion level of orebearing structures. Their deep erosion and long-term denudation resulted in the formation of numerous, often large placers with fine gold, which lost t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e29eb292c49d24289d1d5c74bccf957b
https://doi.org/10.1134/s1819714008050084
https://doi.org/10.1134/s1819714008050084
Publikováno v:
Russian Journal of Pacific Geology. 1:444-453
The relationship between noble metal mineralization and carbonaceous rocks (black shales and brown coals) is considered. We have confirmed the previous conclusions of multistage syn- and epimetamorphic formation of gold-bearing deposits in black shal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d98a12302934b0628c5a2e9a7f11da2
https://doi.org/10.1134/s1819714007050041
https://doi.org/10.1134/s1819714007050041