Zobrazeno 1 - 10
of 63
pro vyhledávání: '"Maya B. Kamenetsky"'
Autor:
Sergey V. Malyshev, Alexei V. Ivanov, Andrey K. Khudoley, Alexander E. Marfin, Vadim S. Kamenetsky, Maya B. Kamenetsky, Olga Yu. Lebedeva
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-10 (2021)
Abstract Mesoproterozoic period included several global tectonic events like break-up of Nuna and formation of Rodinia. However, although Siberia is a significant piece of both supercontinents, Mesoproterozoic time is marked by quiescence of magmatic
Externí odkaz:
https://doaj.org/article/4461e4f152444b83b58f4d1033c3b4b0
Autor:
Maya B. Kamenetsky, Jocelyn McPhie, Jay Thompson, Kathy Ehrig, Roland Maas, Edeltraud Macmillan, Vadim S. Kamenetsky
Publikováno v:
Geology. 49:1312-1316
The origins of many supergiant ore deposits remain unresolved because the factors responsible for such extreme metal enrichments are not understood. One factor of critical importance is the timing of mineralization. However, timing information is com
Polymineralic inclusions in kimberlite-hosted megacrysts: Implications for kimberlite melt evolution
Autor:
Karsten Goemann, D. Graham Pearson, Marina A. Gornova, Igor S. Sharygin, Alexander V. Golovin, Maya B. Kamenetsky, Vadim S. Kamenetsky, Adam Abersteiner
Publikováno v:
Lithos. :310-325
Megacrysts are large (cm to >20 cm in size) mantle-derived crystals, which are commonly entrained by kimberlite magmas, comprising of olivine, orthopyroxene, clinopyroxene, phlogopite, garnet, ilmenite and zircon as common phases. Numerous studies ha
Autor:
Adam Abersteiner, Vadim S. Kamenetsky, Karsten Goemann, Montgarri Castillo-Oliver, Jay Thompson, Maya B. Kamenetsky, AR Cherry, Geoffrey H. Howarth, Andrea Giuliani
Publikováno v:
Lithos. :297-314
The Benfontein kimberlite is a renowned example of a sill complex and provides an excellent opportunity to examine the emplacement and evolution of intrusive kimberlite magmas. We have undertaken a detailed petrographic and melt inclusion study of th
Autor:
Richard E. Ernst, Olga Yu. Belozerova, Vadim S. Kamenetsky, Oleg M. Glazunov, Alexei V. Ivanov, Nikolay V. Bryanskiy, Tamara Yu. Yakich, Alexander E. Marfin, Maya B. Kamenetsky, Sandra L. Kamo, I. F. Gertner, Tatiana A. Radomskaya
Publikováno v:
Journal of Petrology. 62
The initial stage of Rodinia supercontinent break-up occurred at about 750 Ma. It preceded formation of the Irkutsk and Franklin large igneous provinces (LIPs) at 712 ± 2 to 739 ± 8 Ma. These LIPs were emplaced within the formerly connected Laurent
Autor:
Sergey V. Malyshev, Maya B. Kamenetsky, Andrey K. Khudoley, Alexei V. Ivanov, Vadim S. Kamenetsky
Numerous Mesoproterozoic mafic dyke swarms are known in Siberia. The main intrusions are concentrated in the northern part of the platform and in Sette-Daban (southeastern part of Siberia), and single intrusions are known on all the outcrops of the c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d287bf2f2ada52d3eb36ede54e18b0e6
https://doi.org/10.5194/egusphere-egu21-13570
https://doi.org/10.5194/egusphere-egu21-13570
Autor:
V. Savatenkov, Maya B. Kamenetsky, Alexei V. Ivanov, D. Sitkina, O. Labedeva, Vadim S. Kamenetsky, Sergey V. Malyshev, A. Pasenko
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Naomi J. Potter, Anton R. Chakhmouradian, Thomas Rodemann, Maya B. Kamenetsky, Karsten Goemann, Vadim S. Kamenetsky
Publikováno v:
Contributions to Mineralogy and Petrology. 175
The exceptional accumulation of perovskite in the alkaline-ultramafic Afrikanda complex (Kola Peninsula, Russia) led to the study of polymineralic inclusions hosted in perovskite and magnetite to understand the development of the perovskite-rich zone
Autor:
Vadim S. Kamenetsky, Jocelyn McPhie, Kathy Ehrig, AR Cherry, James L. Crowley, Maya B. Kamenetsky
Publikováno v:
Precambrian Research. 315:162-178
The Olympic Dam Breccia Complex (host to the Olympic Dam Cu-U-Au-Ag deposit) is derived largely from granite (Roxby Downs Granite) but includes clasts and domains derived from surficial facies (felsic volcanic rocks and bedded clastic facies). New hi
Autor:
Maya B. Kamenetsky, Adam Abersteiner, Karsten Goemann, Alexander V. Golovin, Vadim S. Kamenetsky
Publikováno v:
Journal of Petrology. 59:1467-1492
The petrologically unique Udachnaya-East kimberlite (Siberia, Russia) is characterised by unserpentinised and H2O-poor volcaniclastic and coherent units that contain fresh olivine, along with abundant alkali-rich carbonates, chlorides, sulphides and