High-titanium gabbroids of the western Dzhugdzhur-Stanovoy superterrane: Age and tectonic setting     

I. V. Buchko  A. A. Sorokin  E. B. Sal’nikova  A. B. Kotov  A. M. Larin  S. D. Velokoslavinsky  Yu. V. Plotkina 《Geochemistry International》2010,48(6):617-620

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Bastnaesite: a promising U-Pb geochronological tool     

Sal’nikova  E. B.  Yakovleva  S. Z.  Nikiforov  A. V.  Kotov  A. B.  Yarmolyuk  V. V.  Anisimova  I. V.  Sugorakova  A. M.  Plotkina  Yu. V. 《Doklady Earth Sciences》2010,430(1):134-136

Doklady Earth Sciences -  相似文献   

Bücher- und Zeitschriftenschau     

H. E. Boeke  Sal 《International Journal of Earth Sciences》1916,7(3-4):174-179

Ohne Zusammenfassung  相似文献   

Bücher- und Zeitschriftenschau     

Sal  St. 《International Journal of Earth Sciences》1914,5(1):78-80

Ohne Zusammenfassung  相似文献   

A new version of the heat flow map of the Urals with paleoclimatic corrections     

I. V. Golovanova  V. N. Puchkov  R. Yu. Sal’manova  D. Yu. Demezhko 《Doklady Earth Sciences》2008,422(1):1153-1156

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Age and tectonic position of granites and volcanics in the eastern Margin of the Selenga-Vitim volcano-plutonic belt     

A. M. Larin  A. B. Kotov  E. B. Sal’nikova  A. A. Sorokin  A. P. Sorokin  A. M. Korshunov  S. D. Velikoslavinskii  S. Z. Yakovleva  Yu. V. Plotkina 《Doklady Earth Sciences》2011,441(1):1502-1507

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Age of the Ilikan Sequence from the Stanovoi Complex of the Dzhugdzhur-Stanovoi Superterrane, Central-Asian Foldbelt     

S. D. Velikoslavinskii  A. B. Kotov  E. B. Sal’nikova  A. M. Larin  A. A. Sorokin  A. P. Sorokin  V. P. Kovach  E. V. Tolmacheva  B. M. Gorokhovskii 《Doklady Earth Sciences》2011,438(1):612-616

This paper presents the results of Sm-Nd isotopic-geochemical and U-Pb geochronological studies of metamorphic (Ilikan Sequence) and associated igneous rocks from the Ilikan lithotectonic zone (terrane) located in the Dzhugdzhur-Stanovoi Superterrane from the Central Asian Foldbelt. The Nd model age, T _Nd(DM), of metamorphic rocks from the Ilikan Sequence is 2.6–3.2 Ga pointing to the likelihood that the lower boundary of their protolith formation probably does not exceed 2.6 Ga. The age of detrital zircons from metasedimentary rocks of the Ilikan Sequence is 2700–2900 Ma, which absolutely agrees with Sm-Nd isotopic-geochemical results. The U-Pb zircon age of metagabbro that intruded the rocks of the Ilikan Sequence and underwent high-temperature amphibolite metamophism with subsequent structural transformations is 2635 ± 4 Ma. The obtained results allow us to conclude that the age of the Ilikan Sequence is 2630–2700 Ma. All this gives grounds to state that the Dzhugdzhur-Stanovoi Superterrane in the Central Asian Foldbelt was formed due to amalgamation of non-Siberian terranes as is assumed for the Argun, Bureya, and Mamynskii terranes of the Amur Superterrane from the Central Asian Foldbelt.  相似文献   

Middle Riphean gneiss granites of the Kokchetav Massif (Northern Kazakhstan): Structural position and age substantiation     

A. A. Tret’yakov  K. E. Degtyarev  A. B. Kotov  E. B. Sal’nikova  K. N. Shatagin  S. Z. Yakovleva  I. V. Anisimova  Yu. V. Plotkina 《Doklady Earth Sciences》2011,440(2):1367-1371

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Upper Crustal Velocity Model for the Southeastern Boundary of the Siberian Platform     

Emanov  A. F.  Polyanskii  P. O.  Sal’nikov  A. S. 《Izvestiya Physics of the Solid Earth》2021,57(3):409-424

Izvestiya, Physics of the Solid Earth - Abstract—Based on the common-mid-point (CMP) seismic data on the 3-DV reference profile, using dynamic conversion of refracted waves into time...  相似文献   

Geodynamic settings and formation conditions of crystalline complexes in the south Altai and south Gobi metamorphic belts     

I. K. Kozakov  A. N. Didenko  P. Ya. Azimov  T. I. Kirnozova  E. B. Sal’nikova  I. V. Anisimova  Ch. Erdenejargal 《Geotectonics》2011,45(3):174-194

The Hercynian mobile belts in Central Asia comprise the Hercynian proper and the Late Hercynian (Indosinian) belts separated by the South Gobi microcontinent, the origin of which is related to the evolution of the South Mongolian and Inner Mongolian basins with the oceanic crust. Crystalline complexes within these belts occur as tectonic sheets of a variety of sizes. At the early stages, the metamorphic grade of these complexes reached conditions of high-temperature subfacies of amphibolite and locally developed granulite facies. In tectonic terms, the Hercynian belt of metamorphic rocks is situated at the margin of the North Asian Caledonian continent and extends from the southeast to the northwest along the southern slope of the Gobi, Mongolian, and Chinese Altai to East Kazakhstan, where metamorphic rocks are localized in the Irtysh Shear Zone. All these rocks are combined into the South Altai metamorphic belt of more than 1500 km in extent. Another belt of isolated outcrops of crystalline rocks conventionally combined into the Indosinian South Gobi metamorphic belt is traced along the junction of the Hercynides with the South Gobi microcontinent. The high-grade metamorphic rocks within both belts are not fragments of an ensialic Caledonian or older basement. These rocks were formed 390–360 and 230–220 Ma ago as a result of the closure of the Tethian South Mongolian and Inner Mongolian oceanic basins (Paleotethys I and Paleotethys II). The spatial position of the South Altai and South Gobi metamorphic belts is caused by the asymmetric structure of the Tethian basins, where active continental margins are expressed most distinctly along their northern parts, while passive margins extend along the southern parts (in present-day coordinates).  相似文献