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Разложение интегралов некоторых классов в обобщенные степенные ряды

Савина, Светлана В., Savina, Svetlana V.

Reply to Vladimir Belikov and Svetlana Burlak

Fleischhauer Jens

Fleischhauer Jens.
Reply to Vladimir Belikov and Svetlana Burlak [Электронный ресурс] / Jens

The Alteration Of Chemical Composition Of Groundwater In The Mines Of Kizel Coal Basin

Sukhorukova Svetlana

E-COMMERCE IN THE BRICS: SIMILARITIES AND DIFFERENCES

Revinova Svetlana

EGFR AND BRCA2 MUTATIONS ASSOCIATED WITH ADENOCARCINOMA OF THE LUNG

Smolina Svetlana, Bakutina Anna

ON AN INDIRECT REPRESENTATION OF EVOLUTIONARY EQUATIONS IN THE FORM OF BIRKHOFF'S EQUATIONS

Budochkina Svetlana, Vu Hue

Ironworks images on the 17th and early 18th century Russian geographic maps as a source for the history of technology

Yurkin Igor, Kalita Svetlana

(chertezh) including a number of maps comprising part of the cartographic heritage of S. U. Remezov

The Labour Share, Government Expenditure and Income Inequality of Post-Soviet Countries

Sergi Bruno S., Balashova Svetlana, Ratner Svetlana

1.86 Ga key paleomagnetic pole from the Murmansk craton intrusions - Eastern Murman Sill Province, NE Fennoscandia: Multidisciplinary approach and paleotectonic applications

Veselovskiy, Roman V., Samsonov, Alexander V., Shcherbakova, Valentina V., Shcherbakov, Valeriy P., Zhidkov, Grigoriy V., Zakharov, Vladimir S., Stepanova, Alexandra V., Salnikova, Ekaterina B., Larionova, Yulia O., Travin, Alexey V., Arzamastsev, Andrey A., Egorova, Svetlana V., Erofeeva, Kseniya G., Stifeeva, Maria V.

remanent magnetization (ChRM) was determined by four independent geochronometers: U-Pb – 1860 ± 4 and 1863

A multiproxy record of sedimentation, pedogenesis, and environmental history in the north of West Siberia during the late Pleistocene based on the Belaya Gora section

Sheinkman, Vladimir S., Sedov, Sergey N., Shumilovskikh, Lyudmila S., Bezrukova, Elena, Dobrynin, Dmitriy, Timireva, Svetlana, Rusakov, Alexey, Maksimov, Fedor

of the buried paleosols are attributed to MIS 5 and MIS 3, as evidenced by U/Th and radiocarbon dates

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