Zobrazeno 1 - 9
of 9
pro vyhledávání: '"E.Yu. Rokosova"'
Publikováno v:
Russian Geology and Geophysics. 63:153-164
—To reveal the formation conditions of synnyrites in the Synnyr alkaline pluton, we studied melt inclusions in the minerals of shonkinites and pseudoleucite syenites, in apatite segregations in pyroxenites, shonkinites, and synnyrites, and in the m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::56e6a53e6f4adfd801149aa30543183b
https://doi.org/10.2113/rgg20204251
https://doi.org/10.2113/rgg20204251
Publikováno v:
Geochemistry International. 56:651-669
Data obtained on lamprophyres from the carbonatite–volcanic unit in the lower horizon of the Tomtor Massif indicate that the rocks and zoned diopside and kaersutite phenocrysts in them are enriched in incompatible elements more significantly than i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::983fddeb208c1056c2a67b59c98e8190
https://doi.org/10.1134/s0016702918070091
https://doi.org/10.1134/s0016702918070091
Publikováno v:
Russian Geology and Geophysics. 58:887-902
The influence of parental melts on the chemical composition of rock-forming minerals of alkaline lamprophyres (monchiquites) referred to as the volcanic series of porphyritic potassic alkaline-ultrabasic rocks was studied in the Tomtor alkaline-ultra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2ba2a1f2c39b9acf8cdf259f60e67e56
https://doi.org/10.1016/j.rgg.2017.07.001
https://doi.org/10.1016/j.rgg.2017.07.001
Publikováno v:
Petrology. 24:608-625
The paper presents data on inclusions in minerals of the least modified potassic lamprophyres in a series of strongly carbonatized potassic alkaline ultramafic porphyritic rocks. The rocks consist of diopside, kaersutite, analcime, apatite, and rare
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f31f4706a4d1a211b5d2bfe6a2b89cf4
https://doi.org/10.1134/s0869591116060047
https://doi.org/10.1134/s0869591116060047
Publikováno v:
Russian Geology and Geophysics. 57:1298-1311
The olivine shonkinites localized among dunites and alkali gabbroids in the northern part of the alkaline ultrabasic Inagli massif (northwestern part of Central Aldan) have been studied. The obtained data on the chemical and trace-element composition
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd0f875a802ae86097008e1663484e37
https://doi.org/10.1016/j.rgg.2016.08.015
https://doi.org/10.1016/j.rgg.2016.08.015
Publikováno v:
Russian Geology and Geophysics. 56:466-475
Inclusions of mineral-forming environments in apatite-containing ijolites and magnetite–phlogopite–apatite ores in carbonatites were studied to elucidate the genesis of apatite mineralization in the Guli alkaline ultramafic carbonatite massif. Pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4052db817abbc18e399e0fd831c204ae
https://doi.org/10.1016/j.rgg.2015.02.007
https://doi.org/10.1016/j.rgg.2015.02.007
Autor:
L. I. Panina, E.Yu. Rokosova
Publikováno v:
Russian Geology and Geophysics. 54:613-626
Dikes of biotitic shonkinites and minettes of the complex Ryabinovyi alkaline massif (Central Aldan) have been studied. The dikes are localized in a neck of K-picrites in the northeast of the massif, which intrudes gold-bearing microcline–muscovite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c0a4394edcbdef1c3596d0c5143a652
https://doi.org/10.1016/j.rgg.2013.04.011
https://doi.org/10.1016/j.rgg.2013.04.011
Publikováno v:
Geochemistry International. 49:120-138
Alkaline-basic dike from the Yllymakh Massif (Central Aldan) has been studied. Its partially crystallized matrix contains corroded phenocrysts of olivine and hypidiomorphic phenocrysts of clinopyroxene and pseudo-, epileucite. It was found that pheno
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::abda11b2f1ea6f0907f346d6ab2130e9
https://doi.org/10.1134/s001670291102008x
https://doi.org/10.1134/s001670291102008x
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