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91.
I. V. Buchko A. A. Sorokin A. A. Rodionov N. M. Kudryashov 《Doklady Earth Sciences》2018,479(2):448-451
U–Pb ID–TIMS zircon analyses of the Dzhigda gabbro–gabbrodiorite Massif (Ilikan block in the southwestern part of the Dzhugdzhur–Stanovoi superterrane) have been carried out. The results demonstrate that the formation of the massif at 244 ± 5 Ma corresponds to one of the stages of formation of the Selenga–Vitim volcano–plutonic belt. The latter stretches along the southeastern margin of the North Asian Craton along its border with the Mongol–Okhotsk fold belt. This indicates that the Selenga–Vitim volcano–plutonic belt along with granitoids and volcanics comprises Permian–Triassic massifs and that this belt is superimposed onto structures of not only the Selenga–Stanovoi terrane but also the Dzhugdzhur–Stanovoi terrane. 相似文献
92.
Belyatsky B. V. Lepekhina E. N. Antonov A. V. Rodionov N. V. Nedosekova I. L. Petrov O. V. Shevchenko S. S. Sergeev S. A. 《Doklady Earth Sciences》2018,481(2):1079-1085
Doklady Earth Sciences - The results of local U–Th–Pb-SIMS-SHRIMP-II analysis of the collection of pyrochlores from Nb rare-metal deposits of the Ilmeny–Vishnevogorsky alkaline... 相似文献
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S. A. Rodionov E. Athanassoula N. Ya. Sotnikova 《Monthly notices of the Royal Astronomical Society》2009,392(2):904-916
We present a new method for constructing equilibrium phase models for stellar systems, which we call the iterative method. It relies on constrained, or guided evolution, so that the equilibrium solution has a number of desired parameters and/or constraints. This method is very powerful, to a large extent due to its simplicity. It can be used for mass distributions with an arbitrary geometry and a large variety of kinematical constraints. We present several examples illustrating it. Applications of this method include the creation of initial conditions for N -body simulations and the modelling of galaxies from their photometric and kinematic observations. 相似文献
95.
V. V. Metallova A. O. Mostrukov A. G. Iosifidi V. P. Rodionov A. N. Khramov 《Geophysical Journal International》1984,76(2):289-298
Summary. The palaeointensity of the geomagnetic field during some ancient polarity transitions as well as and during the Jaramillo event was determined by the method of alternating-field remagnetization. The periods of the secular variation during these transitions were also determined. 相似文献
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Anorogenic magmatic complexes were formed during protoplatformal evolution of the Keivy structure. This evolution ended with
development of aluminous schists, which were derived by deep disintegration and redeposition of the rocks from the lower parts
of the sequence and surrounding of the structure. The anorogenic rocks of the region are represented by the following magmatic
complexes: gabbro-labradorite-latite-monzonite-granites; ophitic gabbro and gabbrodiabases; quartz syenite-alkaline granites;
alkaline and nepheline syenites. The magmatic activity of this period, starting from the emplacement of gabbrolabradorite
massifs and ending with alkaline and nepheline syenite bodies, was caused by ascent of mantle asthenolith, which destructed
the Earth’s crust basement in this area. The anorogenic magmatism of the Keivy structure lasted for no more than few or few
tens of million years. The granitoid subcomplex of the gabbro-labradorite-latite-monzonite-granite complex is dated at 2674
± 6 Ma, which is comparable with an age of alkaline granites of the Ponoy and Beliye Tundry massifs (2673 ± 6 Ma). The considered
complexes are separated in time by intrusion of amphibole-biotite plagiomicrocline granites with an age of 2667 ± 8 Ma. Gabbrolabradorites
of the Shchuch’e Ozero and Tsaga massifs have close ages (2663 ± 7 and 2668 ± 10 Ma, respectively, Bayanova, 2004), but were
formed earlier than granitoids (Bayanova, 2004). Formation of alkaline syenites of the Sakharijok I Massif, which finalized
the Neoarchean anorogenic magmatism of the region, falls in the same interval. During Paleoproterozoic transformations, the
rocks of the Keivy structure were sheared and uranium was introduced in the contact zones of the alkaline granite massifs,
which caused formation of palingenetic melts and subsequent formation of pegmatites in the outer contact zones of the granite
bodies. 相似文献
100.
V. K. Kuz’min V. A. Glebovitskii N. V. Rodionov A. V. Antonov E. S. Bogomolov S. A. Sergeev 《Stratigraphy and Geological Correlation》2009,17(4):355-372
Based on U-Pb dating (SHRIMP-II) of euhedral zircon cores from hypersthene-plagioclase granulites of the Kukhtui Inlier (Okhotsk Massif), their igneous protholith of the basic composition is estimated to be Archean in age (3.7 Ga), which is confirmed by the Sm-Nd measurements. Subsequent tectonothermal events are established to occur 3.3–3.2, 2.8–2.7, and 1.9–1.8 Ga ago. 相似文献