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| 1 | Fragments of oceanic islands in accretion collision areas of Gorny Altai and Salair, southern Siberia, Russia : Early stages of continental crustal growth of the Siberian conti- nent in Vendian-Early Cambrain time显示文摘 | Dobresov N L Buslov M M Uchio Yu | 2004 | Journal of Asian Earth Sci- ences2004，23，： | 1 |
| 2 | Ultraviolet and thermo- stable nonisocyanate polyurethane coatings显示文摘 | Figovsky O L Shapovalov L D Buslov F | 2005 | Surface Coatings In- ternational Part B : Coatings Transactions2005，88，1： | 1 |
| 3 | the Precast Pier 显示文摘 | Valery B Buslov James P Gould Robert C Koch | 1988 | Civil Engineering1988，，12： | 1 |
| 4 | Opening and Tectonic Evolution of the Paleo-Asian Ocean显示文摘 | Dobretsov N Berzin N Buslov M | 1995 | International Geology Review1995，37，4： | 1 |
| 5 | Opening and tectonic evolution of the Paleo-Asian ocean显示文摘 | Dobretsov N L Berzin N A Buslov M M | 1995 | International Geology Review1995，37，： | 1 |
| 6 | Improved reliability of allele-specific PCR 显示文摘 | Imyanitov EN Buslov KG Suspitsin EN | 2002 | Biotechniques2002，33，48： | 1 |
| 7 | Evolution of the Paleo-Asian ocean (Altai-Sayan region, central Asia) and collision of possible Gondwana-derived terranes with the southern marginal part of the Siberian continent 显示文摘 | Buslov M M Saphonova I Yu Watanabe T | 2001 | Geosciences Journal2001，5，3： | 1 |
| 8 | Formation and Palaeozoic evolution of the Gorny-Altai-Altai-Mongolia suture zone (South Siberia): Zircon U/Pb constraints on the igneous record显示文摘 | Glorie S De Grave J Buslov M M | 2011 | Gondwana Research2011，20，23： | 1 |
| 9 | Fragments of oceanic islands in accretion-collision areas of Gorny Ahai and Salair, southern Siberia, Russia, in early stages of continental crustal growth of the Siberian continental in Vendian-Early Cambrian time 显示文摘 | Dobretsov N L Buslov M M Yu U | 2004 | Journal of Asian Earth Sciences2004，23，： | 1 |
| 10 | Ultraviolet and thermostable non-isocyanate polyurethane coatings 显示文摘 | FIGOVSKYO SHAPOVALOVL BUSLOVE | 2005 | Surface Coatings International Part B: CoatingTransacfion2005，88，1： | 1 |
| 11 | The precast pier显示文摘 | Buslov V B Gould J P Koch R C | 1988 | Civil Engineering1988，，12： | 1 |
| 12 | Structural physico-chemistry of cellulose macromolecules: Vibrational spectra and structure of cellulose显示文摘 | ZHBANKOV R G FIRSOV S P BUSLOV D K NIKONENKO N A MARCHEWKA M K RATAJCZAK H | 2002 | J Mol Struct2002，614，13： | 1 |
| 13 | Evolution of the Paleo-Asian Ocean (Altai-Sayan region, Central Asia) and colli- sion of possible Gondwana-derived terranes with the southern mar- ginal part of the Siberiai1 continent 显示文摘 | Buslov M M Safonova I Y Watanabe T | 2001 | Geosciences Journal2001，5，： | 1 |
| 14 | Late Paleozoic faults of the Altai region, Central Asia: tectonic pattern and model of formation 显示文摘 | Buslov M M Watanabe T Fujiwara Y | 2004 | Journal of Asian Earth Sciences2004，23，： | 1 |
| 15 | Meso-and Cenozoic tectonics of lithopheric plate interaction and mantle plumes 显示文摘 | DOBRSTSOV N L BUSLOV M M DELVAUX P | 1996 | International Geology Review1996，38，： | 1 |
| 16 | NBS1 657de15 mutation may contribute only to a limited fraction of breast canc- er cases in Russia显示文摘 | Buslov KG Iyevleva AG Chekmariova EV | 2005 | Int J Cancer2005，114，4： | 1 |
| 17 | Evolution of the Paleo-Asian Ocean (Altai-Sayan Region,Central Asia) and col- lision of possible Gendwana-derived terranes with the southern marginal part of the Siberian continent显示文摘 | Buslov M M Saphonova I Y Watanabe T | 2001 | Geosciences Journal2001，5，3： | 1 |
| 18 | Tectonics and geodynamics of the Central Asianfoldbelt:the role of Late Paleozoic large-amplitude strike-slip faults显示文摘 | Buslov M M | 2011 | Russian Geology and Geophysics2011，52，1： | 1 |
| 19 | Devonian and Lower Cabonif- erous radiolaria from the Chara ophiolite belt, East Kazakhstan 显示文摘 | Iwata K Obut O T Buslov M M | 1996 | News of Osaka Micropaleontologist1996，10，： | 1 |
| 20 | CHEK2 llO0delC mutation is frequent among Russian breast cancer patients 显示文摘 | Chekmariova EV Sokolenko AP Buslov KG | 2006 | Breast Cancer Res Treat2006，100，1： | 1 |
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