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| 1 | Assembly, configuration, and break-up history of Rodinia: A synthesis显示文摘 | Z.X. Li S.V. Bogdanova A.S. Collins A. Davidson B. De Waele R.E. Ernst I.C.W. Fitzsimons R.A. Fuck D.P. Gladkochub J. Jacobs K.E. Karlstrom S. Lu L.M. Natapov V. Pease S.A. Pisarevsky K. Thrane V. Vernikovsky | 2007 | Precambrian Research2007，，1： | 1 |
| 2 | The geodynamic evolution of the Taimyr folded area显示文摘 | Vernikovsky V A | 1996 | Seience1996，217，4565： | 1 |
| 3 | Concerning tectonics and the tectonic evolution of the Arctic显示文摘 | Vernikovsky V A Dobretsov N L Metelkin D V | 2013 | Russian Geology and Geophysics2013，54，： | 1 |
| 4 | Geo- chemistry and age of collision granitoids and metamorphites of the Kara microcontinent (northern Taimyr) 显示文摘 | Vernikovsky V Neimark L Ponomarchuk V | 1995 | Russian Ge- ology and Geophysics1995，36，： | 1 |
| 5 | Petrology and geochemistry of Taimyr Riphean ophiolites显示文摘 | Vernikovsky V A Vernikovskaya A E Chernykh A I | 1996 | Russian Geolology and Geophysics1996，36，： | 1 |
| 6 | Late Mesozoic tectonics of Central Asia based on paleomagnetic evidence 显示文摘 | Metelkin D V Vernikovsky V A Kazansky A Y | 2010 | Gondwana Research2010，18，23： | 1 |
| 7 | Central Taimyr ac-cretionary belt (Arctia Asia) : Meso-Neoproterozoic tectonic evolution and Rodinia breakup 显示文摘 | Vernikovsky V A Vernikovskaya A E | 2001 | Preeambrian Research2001，110，： | 1 |
| 8 | Late Mesozoic Tectonics of Central Asia Based on Paleomagnetic Evidence 显示文摘 | Metelkin D V Vernikovsky V A Kazansky A Y | 2010 | Gondwana Research2010，18，23： | 1 |
| 9 | Mesozoic-Cenozoic volcanism and geodynamic events in the Central and Eastern Arctic 显示文摘 | Dobretsov N L Vernikovsky V A Karyakin Yu V | 2013 | Russian Geology and Geo- physics2013，54，： | 1 |
| 10 | The Svalbrd-Kala Plates Junction: Structure and Geodynamie History 显示文摘 | Shipilov E V Vernikovsky V A | 2010 | Russian Geology and Geophysics2010，51，： | 1 |
| 11 | Con- cerning tectonics and the tectonic evolution of the Arctic 显示文摘 | Vernikovsky V A Dobretsov N L Metelkin D V | 2013 | Russian Geology and Geophysics2013，54，8： | 1 |
| 12 | Petrology and Geochemistry of the Riphean Ophiolites in North Taimyr显示文摘 | Vernikovsky V A Vernikovskaya A E Chernykh A I | 1996 | Geol Geofiz1996，37，1： | 1 |
| 13 | Paleozoic History of the Kara Microcontincnt and Its Relation to Siberia and Baltica; Paleomag- netism, Paleogeography and Tectonics 显示文摘 | Metelkin D V Vernikovsky V A Kazansky A Yu | 2005 | Tectono- physics2005，398，： | 1 |
| 14 | Riphean and Paleozoic Metamorphic Complexes of the Taimyr Foldbelt: Condition of For- mation显示文摘 | Vernikovsky V | 1995 | Petrol1995，3，： | 1 |
| 15 | Late Mesozoic tectonics of Central Asia based on paleomagnetic evidence显示文摘 | Metelkin D V Vernikovsky V A Kazansky A Y | 2010 | Gondwana Research2010，18，23： | 1 |
| 16 | Neoprotero- zoic to early ordovician evolution of the paleo-asian ocean: Implications to the break-up of rodinia显示文摘 | Dobretsov NL Buslov MM Vernikovsky VA | 2003 | Gondwana Re- search2003，6，： | 1 |
| 17 | The Svalbard - Kara plates junction: Structure and geodynamic history 显示文摘 | Shipilov E V Vernikovsky V A | 2010 | Russian Geology and Geophysics2010，51，： | 1 |
| 18 | Neoproterozoic to Early Ordovician evolution of the Paleo-Asian Ocean: implications to the break-up of Rodinia显示文摘 | Nikolay L Dobretsov Mikhail M Buslov Valery A Vernikovsky | 2003 | Gondwana Research2003，6，2： | 1 |
| 19 | Tectonic evolution of the Siberian paleocontinent from the Neoproterozoic to the Late Mesozoic: paleomagnetic record and reconstructions 显示文摘 | METELKIN D V VERNIKOVSKY V A KAZANSKY A Y | 2012 | Russian Geology and Geophysics2012，53，7： | 1 |
| 20 | Geological and Geochemical Features of the Neoproterozoic Ophiolites Along the Folded Siberian Platform Margin显示文摘The data of the last decade investigations of ophiolites in western m argin of Siberian platform were summarized. The study of geology, geoche mistry and geochronology show that the interrupted ophiolitic belt of Neoprotero zoic age is 2000 km long, from the Taimir Peninsula to the Northern Transbaikali a Region through the Yeniseyski Khryazh and the Sayanskii Range. These studies i ndicated that the major differences of the Neoproterozoic ophiolites from younge r Phanerozoic ophiolite complexes are as follows: 1) occurrence of komatiite and picritie-like, high-magnesium rocks among the ophiolite volcanics; 2) ophioli te volcanics with both MOR and island-arc tholeiites; 3) ophiolite sequence where sheeted dikes and layered complex ('low gabbro') are usually absent. These pecu larities indicate that the Neoproterozoic ophiolites of Eastern Siberia were gen erated at suprasubduction environment and the Neoproterozoic oceanic crust was n ot as thick as Phanerozoic one. | Konnikov Eduard G. (Institute of Experimental Mineralogy, 142432 Chernogolovka, Moscow D istr., Russia) Tsygankov Andrey A. (Geological Institute of Siberian Branch of RAS, Sakhyanovoy 6a, 6700 47 Ulan-Ude, Russia) Vernikovsky Valery A. (Institute of | 1999 | Global Geology1999，4，2： | 0 |
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