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| 1 | Evolution of the Mongol Okhotsk ocean as constrained by new paleomagnetic data from the Mongol Okhotsk suture zone, Siberia 显示文摘 | Kravchinsky V A Cogne J-P Harbert W P | 2002 | Geophysical Journal International2002，148，： | 1 |
| 2 | Evolution of the Mongol-Okhotsk Ocean as Con- strained by New Palaeomagnetic Data from the Mon- gol-Okhotsk Suture Zone, Siberia 显示文摘 | Kravchinsky V A Cogne J P Harbert W P | 2002 | Geophysical Journal International2002，148，： | 1 |
| 3 | E-volution of the Mongol-Okhotsk Suture Zone, Siberia显示文摘 | Kravchinsky V A Cogne J P Harbert W P | 2002 | Geophysical Journal International?2002，148，1： | 1 |
| 4 | Paleomagnetic Dating of Phanerozoic Kim-berlites in Siberia显示文摘 | BLANCO D KRAVCHINSKY V A KONSTANTINOV K M | 2013 | Journal of Applied Geophysics2013，88，： | 1 |
| 5 | Phanerozoic hot spot traces and paleogeographic reconstructions of the Siberian continent based on interaction with the African large low shear velocity province 显示文摘 | Kuzmin M I Yarmolyuk V V Kravchinsky V A | 2010 | Earth-Science Reviews2010，102，： | 1 |
| 6 | Evolution of the evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia显示文摘 | Kravchinsky V A Cogne J P Harbert W P | 2002 | Geophysical Journal International2002，148，1： | 1 |
| 7 | Palaeomagnetism of east Siberian traps and kimberlites:two new poles and palaeogeographic reconstructions at about 360 and 250 Ma显示文摘 | Kravchinsky V A Konstantinov K M Courtillot V | 2002 | Geophysical Journal International2002，148，： | 1 |
| 8 | Late Ju- rassic-Early Cretaceous closure of the Mongol-Okhotsk Ocean demonstrated by new Mesozoic palaeomagnetic re- suits from the Trans-Baikal area (SE Siberia) 显示文摘 | Cogn6 J P Kravchinsky V A Halim N | 2005 | Ge- ophysical Journal International2005，163，2： | 1 |
| 9 | Evo- lution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk su- ture zone, Siberia 显示文摘 | Kravchinsky V A Cogn6 J P Harbert W P | 2002 | Geophysical Journal Internation- al2002，148，1： | 1 |
| 10 | Evolution of the Mongol-Okhotsk ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia 显示文摘 | Kravchinsky V A Congne J P Harbert W P | 2002 | Geophysical Journal International2002，148，： | 1 |
| 11 | Paleozoic large igneous provinces of Northern Eurasia:correlation with mass extinction events显示文摘 | Kravchinsky V A | 2012 | Global and Planetary Change2012，86，： | 1 |
| 12 | Evo- lution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk su- ture zone, Siberia 显示文摘 | Kravchinsky V A Cogne J P Harbert W P | 2002 | Geophysical Journal Interna- tional2002，148，1： | 1 |
| 13 | Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone,Siberia显示文摘 | Kravchinsky V A CognéJ P Harbert W P | 2002 | Geophysical Journal International2002，148，1： | 1 |
| 14 | A palaeomagnetic study from the Mongol–Okhotsk region: rotated Early Cretaceous volcanics and remagnetized Mesozoic sediments显示文摘 | Nadir Halim Vadim Kravchinsky Stuart Gilder Jean-Pascal Cogné Maxim Alexyutin Andrey Sorokin Vincent Courtillot Yan Chen | 1998 | Earth and Planetary Science Letters1998，，3： | 1 |
| 15 | Paleozoic large igneous provinces of Northem Eurasia: Correlation with mass extinction events 显示文摘 | Kravchinsky V A | 2012 | Global and Planetary Change2012，8687，： | 1 |
| 16 | A Palaeomagnetic study from the Mongol-Okhotsk region, rotated Early Cretaceous volcanics and remagnetized Mesozoic sediments显示文摘 | Kravchinsky V Gilaer S | | Earth and Planetary Science Letters0，1998，： | 1 |
| 17 | Paleomonsoon route reconstruction along a W-E transect in the Chinese Loess Plateau using the anisotropy of magnetic susceptibility:Summer monsoon model显示文摘 | Zhang R Kravchinsky V A Zhu R X | | 0，，3： | 1 |
| 18 | Paleozoic large igneous provinces of Northern Eurasia: Correlation with mass extinction events 显示文摘 | Kravchinsky V A | 2012 | Global and Planetary Change2012，86，： | 1 |
| 19 | Phanerozoic hot spot traces and paleogeographic of the Siberian continent based on interaction with the African large low shear velocity province 显示文摘 | Kuzmin M I Yarmolyuk V V Kravchinsky VA | 2010 | Earth-Science Reviews2010，102，： | 1 |
| 20 | The northern Qiangtang Block rapid drift during the Triassic Period:Paleomagnetic evidence显示文摘As one of the pivotal Gondwana-derived blocks,the kinematic history of the northern Qiangtang Block(in the Tibetan Plateau)remains unclear,mainly because quantitative paleomagnetic data to determine the paleoposition are sparse.Thus,for this study,we collected 226 samples(17 sites)from Triassic sedimentary rocks in the Raggyorcaka and Tuotuohe areas of the northern Qiangtang Block(NQB).Stepwise demagnetization isolated high temperature/field components from the samples.Both Early and Late Triassic datasets passed field tests at a 99%confidence level and were proved to be primary origins.Paleopoles were calculated to be at 24.9°N and 216.5°E with A95=8.2°(N=8)for the Early Triassic dataset,and at 68.1 N,179.9 E with A(95)=5.6°(N=37)for the Late Triassic,the latter being combined with a coeval volcanic dataset published previously.These paleopoles correspond to paleolatitudes of14.3°S±8.2°and 29.9 N15.6°,respectively.Combining previously published results,we reconstructed a three-stage northward drift process for the NQB.(1)The northern Qiangtang Block was located in the subtropical part of the southern hemisphere until the Early Triassic;(2)thereafter,the block rapidly drifted northward from southern to northern hemispheres during the Triassic;and(3)the block converged with the Eurasian continent in the Late Triassic.The^4800 km northward movement from the Early to Late Triassic corresponded to an average motion rate of^11.85 cm/yr.The rapid drift of the NQB after the Early Triassic led to a rapid transformation of the Tethys Ocean. | Yanan Zhou Xin Cheng Yiying Wu Vadim Kravchinsky Ruiqi Shao Weijie Zhang Bitian Wei Ruiyao Zhang Fanrong Lu Hanning Wu | 2019 | Geoscience Frontiers2019，10，6： | 1 |
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