Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Evgeny I Nikolenko"'
Autor:
Dmitriy I. Rezvukhin, Evgeny I. Nikolenko, Igor S. Sharygin, Olga V. Rezvukhina, Maria V. Chervyakovskaya, Andrey V. Korsakov
Publikováno v:
Mineralogical Magazine. 86:60-77
Pyrope xenocrysts (N = 52) with associated inclusions of Ti- and/or Cr-rich oxide minerals from the Aldanskaya dyke and Ogonek diatreme (Chompolo field, southeastern Siberian craton) have been investigated. The majority of xenocrysts are of lherzolit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1eb4721a7ed69c95434ecba3a55d5983
https://doi.org/10.1180/mgm.2021.89
https://doi.org/10.1180/mgm.2021.89
Autor:
Evgeny I. Nikolenko, Konstantin V. Lobov, Alexey M. Agashev, Nikolay S. Tychkov, Maria V. Chervyakovskaya, Igor S. Sharygin, Anna M. Nikolenko
Publikováno v:
Minerals, Vol 10, Iss 10, p 886 (2020)
The alkaline igneous rocks of the Chompolo field (Aldan shield, Siberian craton), previously defined as kimberlites or lamproites, are more correctly classified as low-Ti lamprophyres. The emplacement age of the Ogonek pipe (137.8 ± 1.2 Ma) and the
Externí odkaz:
https://doaj.org/article/2087e1061387476d85dc1f582718a26d
Autor:
D. S. Yudin, Nikolay V. Vladykin, Hilary Downes, Evgeny I Nikolenko, Igor Ashchepkov, N.S. Medvedev
Publikováno v:
Journal of Earth System Science. 130
Lamprophyric (lamproitic) diatremes in Chompolo field, NE Aldan shield, Siberia dated 132 Ma contain abundant mantle xenocrysts studied by EPMA and LA-ICP-MS. The deepest rocks ~6.5 GPa determined with thermobarometry are phlogopite eclogites. Thermo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7fcd023ea57b33ea02d0c723bd3d4400
https://doi.org/10.1007/s12040-021-01694-z
https://doi.org/10.1007/s12040-021-01694-z