排序方式: 共有23条查询结果,搜索用时 15 毫秒
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Ivashchenko V. I. Bushmin S. A. Ruchyev A. M. Kornakov A. S. Bogomolov E. S. Savva E. V. Ivanov M. V. Tytyk V. M. Frolov P. V. 《Doklady Earth Sciences》2018,480(2):804-809
One unsolved problem of Archean metallogeny of the Russian part of the Fennoscandian Shield is related to the period of formation of orogenic gold deposits, the age of which was previously considered Early Proterozoic. Comprehensive studies identified the complex evolution of ores from the Novye Peski deposit and the first Neoarchean Sm–Nd isochron isotopic age (2583 ± 16 Ma) of the formation of orogenic gold of the Karelian Craton. A significant positive εNd(t) value of +4.7 of gold-bearing metasomatites probably points to the link between the ore-forming fluid and the deep mantle source.
相似文献5.
The proposed PT grid of mineral facies of metamorphic rocks, which retains the commonly adopted nomenclature (greenschist, epidote-amphibolite, amphibolite, granulite, glaucophane-schist, and eclogite facies), is based on original calculations and the published calculated and experimental data on mineral equilibria. To validate the facies and subfacies PT boundaries, the mineral equilibria in metapelitic and metabasic rocks have been used. 相似文献
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Yu. M. Lebedeva V. A. Glebovitskii S. A. Bushmin E. S. Bogomolov E. V. Savva K. I. Lokhov 《Doklady Earth Sciences》2010,432(1):602-605
The Sm-Nd isotope-chronological method is used for the first time to investigate the whole rock and rock-forming minerals
from metasomatic sillimanite orthopyroxene rocks in the Por’ya Guba nappe of the Lapland granulite belt. As a result isochrone
values of the age are obtained, which allows estimate the minimum time intervals that have passed from the moment of formation
of the investigated rocks. They indicate that peak conditions of collision metamorphism in fluid-permeable shear zones of
the LGB occurred in the Paleoproterozoic Svekofennian age when high-temperature high-pressure sillimanite-orthopyroxene metasomatic
rocks were formed. The obtained data make it possible to assume that, with regard to the measurement errors, high-pressure
metasomatism did not last over 10 Ma, and this process did not coincide in time with older medium pressure metamorphism. 相似文献
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Skublov S. G. Bushmin S. A. Kuznetsov A. B. Li X.-H. Li Q.-L. Levashova E. V. Savva E. V. 《Doklady Earth Sciences》2020,491(2):247-252
Doklady Earth Sciences - For the first time, the isotopic composition of oxygen, the content of trace elements, and the U–Pb zircon age were determined for kyanite–gedrite metasomatites... 相似文献
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