排序方式： 共有34条查询结果，搜索用时 15 毫秒
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Gordeev V. V. Shevchenko V. P. Korobov V. B. Kochenkova A. I. Starodymova D. P. Belorukov S. K. Lokhov A. S. Yakovlev A. E. Chultsova A. L. Zolotykh E. O. Lobkovsky L. I. 《Doklady Earth Sciences》2021,500(1):787-793
Doklady Earth Sciences - The results of four years of continuous investigations (from May 2015 through April 2019) of the elemental composition of the water of the Northern Dvina River are... 相似文献
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Gordeev V. V. Dara O. M. Alekseeva T. N. Kochenkova A. I. Boev A. G. Lokhov A. S. Belorukov S. K. 《Oceanology》2020,60(3):384-392
Oceanology - The paper presents the first results of a study of seasonal variations in the grain size distribution and mineral compositions of suspended particulate matter (SPM) of the Northern... 相似文献
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Oceanology - The article presents the results of studying the distribution and composition of dispersed sedimentary matter (suspended particulate matter, SPM) in the Barents Sea water column. The... 相似文献
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Malitch K. N. Lokhov D. K. Proskurnin V. F. Puchkov V. N. Badanina I. Yu. Chervyakovskaya M. A. 《Doklady Earth Sciences》2020,492(1):346-350
Doklady Earth Sciences - This study utilized SHRIMP, LA MC–ICP–MS and ID-TIMS analytical techniques and presents for the first time U–Pb age, Lu-Hf-isotope features of zircon and... 相似文献
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L. Yu. Sergeeva N. I. Gusev K. I. Lokhov V. A. Glebovitskii 《Geochemistry International》2017,55(4):380-383
The Hf-Nd isotope systematics was used to determine the genesis of zircons from granulites of the Daldyn Group of the Anabar Shield. Obtained age of magmatic crystallization for biotite–hypersthene crystalline schists and garnet amphibolites agree with position of zircons within terrestrial array. Magmatic genesis of plagiogranite neosome under granulite conditions was established for leucocratic plagiogneisses. 相似文献
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S. B. Lobach-Zhuchenko V. V. Balaganskii M. Yu. Koreshkova K. I. Lokhov Sh. K. Baltybaev L. M. Stepanyuk Yu. S. Egorova S. A. Sergeev I. N. Kapitonov O. L. Galankina E. S. Bogomolov N. G. Berezhnaya V. V. Sukach 《Doklady Earth Sciences》2017,474(2):700-705
This report presents data on the geological structure and location of the orthopyroxenite inclusion in gneissic enderbites of the Bug granulite–gneiss domain. Three stages of orthopyroxenite formation were identified on the basis of studies of the mineral composition along with the U–Pb and Lu–Hf isotope systems of zircons. 相似文献
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S. B. Lobach-Zhuchenko T. V. Kaulina K. I. Lokhov Yu. S. Egorova S. G. Skublov O. L. Galankina A. V. Antonov 《Geology of Ore Deposits》2017,59(8):663-676
This paper presents the results of a complex study (morphology of grains, internal texture in cathodoluminescence and backscattered electrons, microprobe analysis, Lu–Hf data) of five groups (generations) of zircon crystals differing in age and separated from the same granulite sample pertaining to the Bug River Complex of the Ukrainian Shield. The data show that the oldest zircon crystals of the first group (3.74 Ga in age) are xenogenic and initially crystallized from a granitic melt; zircon of the second group (3.66 Ga) formed from a mafic melt contaminated by felsic country rocks. The third group (3.59 Ga) is represented by zircons that formed about 100 Ma later than the second group under conditions of granulite-facies metamorphism and with the participation of fluid-saturated anatectic melt. Two Paleoproterozoic zircon groups (~2.5 and 2.1 Ga) also formed under granulite-facies conditions; to a certain extent, their structure and composition were controlled by fluid. The geochemistry of all zircon generations provides evidence for their crystallization in the continental crust, but from the sources differing in the contribution of mantle-derived material and in oxygen fugacity. 相似文献
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