Zobrazeno 1 - 10
of 26
pro vyhledávání: '"E. E. Kolova"'
Publikováno v:
Bulletin of the North-East Science Center. :13-29
The authors briefly characterize the geology and structure of the Shtokovoye ore field attached to the area where the Khurchan-Orotukan zone of tectonic-magmatic activation overlays the structures of the Yana-Kolyma ore-bearing belt. Studied are mine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aea612f85b488275bcc5395d8c89bbbc
https://doi.org/10.34078/1814-0998-2021-1-13-29
https://doi.org/10.34078/1814-0998-2021-1-13-29
Publikováno v:
Geology of Ore Deposits. 63:34-53
The Burgali deposit is located in the Paleozoic Kedon volcanic belt (KVB) within the Omolon cratonic terrane. The orebodies of the Burgali deposit are veined and stockwork-type. The studies of the wallrock metasomatites demonstrate that the erosional
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5625b9d38baaf113a56e03cbb7d4e503
https://doi.org/10.1134/s1075701520060082
https://doi.org/10.1134/s1075701520060082
Autor:
N. V. Berdnikov, E. E. Kolova, Khabarovsk Geophysics n. a. Yu. A. Kosygin, G. O. Polzunenkov, A. N. Glukhov, V. V. Akinin
Publikováno v:
Bulletin of the North-East Science Center. :3-10
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1c378abece5f18a71eaa2beba58daa4
https://doi.org/10.34078/1814-0998-2020-1-3-10
https://doi.org/10.34078/1814-0998-2020-1-3-10
Autor:
A. V. Alshevsky, E. E. Kolova, V. V. Akinin, V. M. Kuznetsov, N. E. Savva, V. T. Mamatyusupov, N. A. Goryachev, G. O. Polzunenkov
Publikováno v:
Bulletin of the North-East Science Center. :3-8
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86db085076eb2502c81b8107b7c182fc
https://doi.org/10.34078/1814-0998-2019-4-3-8
https://doi.org/10.34078/1814-0998-2019-4-3-8
Publikováno v:
Геология рудных месторождений. 61:52-74
As a potentially large Ag-Au epithermal deposit, Primorskoye comprises the following three areas: Kholodny, Spiridonych, and Teply. This deposit is located in the Omsukchan district of the Magadan Region, where similar deposits, including Dukat, Lunn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3fc6bd72d1b3c36dc4e5eaf9b1c45870
https://doi.org/10.31857/s0016-777061152-74
https://doi.org/10.31857/s0016-777061152-74
Publikováno v:
Geology of Ore Deposits. 61:50-73
The potentially large Primorskoe epithermal Au-Ag deposit is represented by three areas: the Kholodnyi, Spiridonych, and Teplyi. It is located in the Omsukchan district of Magadan oblast, where mining is carried out at the largely similar Dukat, Lunn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aaa297e9e9cffb062de4d103148d7f00
https://doi.org/10.1134/s1075701519010069
https://doi.org/10.1134/s1075701519010069
Publikováno v:
Journal of Volcanology and Seismology. 12:359-378
This paper considers the geochemistry and conditions of generation for the Mesozoic Au–Ag epithermal deposits in the Okhotsk–Chukchi volcanic–plutonic belt (OChVB) in Northeast Russia. We provide new data on the composition and concentrations o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0ff1aece2d386fdb4bd58edf1f65c95
https://doi.org/10.1134/s0742046318060088
https://doi.org/10.1134/s0742046318060088
Publikováno v:
Geology of Ore Deposits. 60:527-545
The Dvoinoe Au-Ag low-sulfide epithermal deposit is located in the Ilirnei ore district (western Chukotka) within the outer zone of the Okhotsk–Chukotka volcanic belt (OChVB). The paper considers the results of geological–structural, mineralogica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c1097888d9a2350ecc5f039611e47f9
https://doi.org/10.1134/s1075701518060053
https://doi.org/10.1134/s1075701518060053
Publikováno v:
Doklady Earth Sciences. 481:869-872
The mineralogical–geochemical and thermobarogeochemical features of the Teploe Ag–Au epithermal deposit are considered. The dissolution and redeposition of ore minerals are a result of thermal metamorphism. The redistribution of Ag leads to the f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f647de25e17f61f748fa21521bf9c3a3
https://doi.org/10.1134/s1028334x18070310
https://doi.org/10.1134/s1028334x18070310
Publikováno v:
Doklady Earth Sciences. 478:166-170
The results of thermobaric geochemical study of ores of the Dvoinoye epithermal Au–Ag deposit are considered. Study of the fluid inclusions has shown that the ores were formed from low-salinity hydrothermal solutions with Na, Ka, and Mg chlorides a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::48618d766ccf75bc873c96be292bf587
https://doi.org/10.1134/s1028334x18020149
https://doi.org/10.1134/s1028334x18020149