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| 1 | Evidence of Solar Variation in Tree-Ring-Based Climate Reconstructions显示文摘 | M.G. Ogurtsov G.E. Kocharov M. Lindholm J. Meril?inen M. Eronen Yu.A. Nagovitsyn | 2002 | Solar Physics2002，，2： | 1 |
| 2 | First experience with SND calorimeter at VEPP-2000 collider显示文摘 | M.N. Achasov D.E. Berkaev A.G. Bogdanchikov D.A. Bukin I.A. Koop A.A. Korol S.V. Koshuba D.P. Kovrizhin A.V. Otboev E.A. Perevedentsev Yu.A. Rogovsky A.L. Romanov P.Yu. Shatunov Yu.M. Shatunov D.B. Shwartz A.A. Valkovich I.M. Zemlyansky | 2008 | Nuclear Inst. and Methods in Physics Research, A2008，，1： | 1 |
| 3 | SND tracking system—Tests with cosmic muons显示文摘 | V.M. Aulchenko A.G. Bogdanchikov A.A. Botov A.D. Bukin D.A. Bukin T.V. Dimova V.P. Druzhinin P.V. Filatov V.B. Golubev A.G. Kharlamov A.A. Korol S.V. Koshuba A.E. Obrazovsky E.V. Pakhtusova V.M. Popov S.I. Serednyakov A.A. Sirotkin I.K. Surin Yu.A. Tikhon | 2008 | Nuclear Inst. and Methods in Physics Research, A2008，，1： | 1 |
| 4 | Computing of gas flows in micro- and nanoscale channels on the base of the Boltzmann Kinetic equation显示文摘 | Yu.A. Anikin E.P. Derbakova O.I. Dodulad Yu.Yu. Kloss D.V. Martynov O.A. Rogozin P.V. Shuvalov F.G. Tcheremissine | 2010 | Procedia Computer Science2010，，1： | 1 |
| 5 | Nanostructured alumina as a cathode of organic light-emitting devices显示文摘 | A.V. Kukhta G.G. Gorokh E.E. Kolesnik A.I. Mitkovets M.I. Taoubi Yu.A. Koshin A.M. Mozalev | 2002 | Surface Science2002，，： | 1 |
| 6 | Comparative analysis of genes encoding key steroid core oxidation enzymes in fast-growing Mycobacterium spp. strains显示文摘 | E.Yu. Bragin V.Yu. Shtratnikova D.V. Dovbnya M.I. Schelkunov Yu.A. Pekov S.G. Malakho O.V. Egorova T.V. Ivashina S.L. Sokolov V.V. Ashapkin M.V. Donova | 2013 | Journal of Steroid Biochemistry and Molecular Biology2013，，： | 1 |
| 7 | Phlogopite in mantle xenoliths and kimberlite from the Grib pipe,Arkhangelsk province,Russia:Evidence for multi-stage mantle metasomatism and origin of phlogopite in kimberlite显示文摘We present petrography and mineral chemistry for both phlogopite,from mantle-derived xenoliths (garnet peridotite,eclogite and clinopyroxene-phlogopite rocks) and for megacryst,macrocryst and groundmass flakes from the Grib kimberlite in the Arkhangelsk diamond province of Russia to provide new insights into multi-stage metasomatism in the subcratonic lithospheric mantle (SCLM) and the origin of phlogopite in kimberlite.Based on the analysed xenoliths,phlogopite is characterized by several generations.The first generation (Phl1) occurs as coarse,discrete grains within garnet peridotite and eclogite xenoliths and as a rock-forming mineral within clinopyroxene-phlogopite xenoliths.The second phlogopite generation (Phl2) occurs as rims and outer zones that surround the Phl1 grains and as fine flakes within kimberlite-related veinlets filled with carbonate,serpentine,chlorite and spinel.In garnet peridotite xenoliths,phlogopite occurs as overgrowths surrounding garnet porphyroblasts,within which phlogopite is associated with Cr-spinel and minor carbonate.In eclogite xenoliths,phlogopite occasionally associates with carbonate bearing veinlet networks.Phlogopite,from the kimberlite,occurs as megacrysts,macrocrysts,microcrysts and fine flakes in the groundmass and matrix of kimberlitic pyroclasts.Most phlogopite grains within the kimberlite are characterised by signs of deformation and form partly fragmented grains,which indicates that they are the disintegrated fragments of previously larger grains.Phl1,within the garnet peridotite and clinopyroxeneephlogopitexenoliths,is characterised bylow Ti and Cr contents (TiO2<1 wt.%,Cr2O3<1 wt.% andMg#=100×Mg/(MgtFe)>92) typical of primary peridotite phlogopite in mantle peridotite xenoliths from global kimberlite occurrences.They formed during SCLM metasomatism that led to a transformation from garnet peridotite to clinopyroxene-phlogopite rocks and the crystallisation of phlogopite and high-Cr clinopyroxene megacrysts before the generation of host-kimberlite magmas.One of the possible processes to generate low-Ti-Cr phlogopite is via the replacement of garnet during its interaction with a metasomatic agent enriched in K and H2O.Rb-Sr isotopic data indicates that the metasomatic agent had a contribution of more radiogenic source than the host-kimberlite magma.Compared with peridotite xenoliths,eclogite xenoliths feature low-Ti phlogopites that are depleted in Cr2O3 despite a wider range of TiO2 concentrations.The presence of phlogopite in eclogite xenoliths indicates that metasomatic processes affected peridotite as well as eclogite within the SCLM beneath the Grib kimberlite.Phl2 has high Ti and Cr concentrations (TiO2 > 2 wt.%,Cr2O3 > 1 wt.% and Mg#=100 × Mg/(Mg + Fe)< 92) and compositionally overlaps with phlogopite from polymict breccia xenoliths that occur in global kimberlite formations.These phlogopites are the product of kimberlitic magma and mantle rock interaction at mantle depths where Phl2 overgrew Phl1 grains or crystallized directly from stalled batches of kimberlitic magmas.Megacrysts,most macrocrysts and microcrysts are disintegrated phlogopite fragments from metasomatised peridotite and eclogite xenoliths.Fine phlogopite flakes within kimberlite groundmass represent mixing of high-Ti-Cr phlogopite antecrysts and high-Ti and low-Cr kimberlitic phlogopite with high Al and Ba contents that may have formed individual grains or overgrown antecrysts.Based on the results of this study,we propose a schematic model of SCLM metasomatism involving phlogopite crystallization,megacryst formation,and genesis of kimberlite magmas as recorded by the Grib pipe. | A.V. Kargin L.V. Sazonova A.A. Nosova N.M. Lebedeva Yu.A. Kostitsyn E.V. Kovalchuk V.V. Tretyachenko Ya.S. Tikhomirova | 2019 | Geoscience Frontiers2019，10，5： | 1 |
| 8 | On the nature of “functional groups” in non-functionalized hypercrosslinked polystyrenes显示文摘 | M.P. Tsyurupa Z.K. Blinnikova Yu.A. Davidovich S.E. Lyubimov A.V. Naumkin V.A. Davankov | 2011 | Reactive and Functional Polymers2011，，12： | 1 |
| 9 | Role of back-arc tectonics in the origin of subduction magmas: new Sr, Nd, and Pb isotope data from Middle Miocene lavas of Kunashir Island (Kurile Island Arc)显示文摘 | A.Yu. Martynov Yu.A. Martynov A.V. Rybin J.-I. Kimura | 2015 | Russian Geology and Geophysics2015，，3： | 1 |
| 10 | A new method for solving dynamic problems of fractional derivative viscoelasticity显示文摘 | Yu.A. Rossikhin M.V. Shitikova | 2000 | International Journal of Engineering Science2000，，2： | 1 |
| 11 | Phase Separation of an Electrolyte during Etching and Sedimentation of Metals on a Surface of a Ferromagnetic Metal Ball in an External Magnetic Field显示文摘 | Gorobets Yu.I. Gorobets O.Yu. Kyba A.A. Legenkiy Yu.A. | 2015 | 材料科学与工程(中英文A版)2015，5，3： | 0 |
| 12 | Identification of Time-of-Flight spectra for Isochronous Mass Measurements显示文摘The Isochronous Mass Spectrometry (IMS) developed at GSI is a very effcient method for direct mass measurements of short-lived nuclides. By taking a recent IMS experiment as an example, the identification procedure of the Time-of-Flight (TOF) spectrum measured in this experiment is discussed. | 孙保华 H. Geissel M. Hausmann C. Kozhuharov R. Knbel Yu.A. Litvinov 孟杰 Z. Patyk T. Radon C. Scheidenberger | 2009 | Chinese Physics C2009，33，S1： | 0 |
| 13 | The scientific basics of aluminium containing raw materials treatment by the chlorous method显示文摘 | Vetchinkina T.N. Lainer Yu.A. Rozhkov D.Yu. Tuzhilin A.S. | 2005 | 广东有色金属学报2005，15，2： | 0 |
| 14 | Diffusion of hydrogen and its isotopes in BCC-metals显示文摘 | Kashlev Yu.A. Sadykov N.M. Vinogradova N.A. | 2005 | 广东有色金属学报2005，15，2： | 0 |
| 15 | UN核燃料中氧杂质的第一性原理模型显示文摘本文报导了氮化铀(UN)核燃料中氧(O)杂质的第一性原理(VASP)超点阵计算结果,这些O杂质存放在间隙四面体中或者置换主体氮(N)离子。在后丽一种情况中,O原子与N空位匹配良好,不会产生晶格畸变。这些O置换杂质只轻微地影响了相邻铀(U)和N空位形成能。在间隙或置换位置,O原子都会吸引额外的电子从而转化为负离子。O嵌入已经存在的N空位比嵌入间隙位置更有利于能量的增加。O杂质能使计算一氮化铀中N分布的电子态密度投影(DOS)图中低能量的一端产生一个额外的峰值,该峰值可用来通过紫外光电子能谱光谱学的方法鉴定O。本文还比较了用来计算UN和假定的同构型氧化铀(UO)的DOS图。O的溶解和结合能都为负,表明O渗入UN燃料是有利于能量增加的。间隙O离子的迁移能估计为2.8eV. | E.A. Kotomin Yu.A. Mastrikov 魏连峰(译) 陈路(校) | 2010 | 国外核动力2010，31，6： | 0 |
| 16 | The Nature of Gamma-ray Bursts in the Framework of the Byuon Theory显示文摘Two models of gamma-ray bursts using the theory of byuons (TB) are considered.This theory describes a “life” of special unobservable discrete objects from which the surrounding space and the world of ultimate particles are formed.Basic axioms and some conclusions of this theory are discussed.It is shown that basic problems with nature of gamma-rays bursts can be solved in the framework of this theory not only for bursts connected with supernova explosions but also for those without explosions. | Yu.A. Baurov I.F. Malov | 2018 | Expert Opinion on Astronomy & Astrophysics2018，2，1： | 0 |
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