gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2012-3-4-0084gtcrust-175Research ArticleОБСУЖДЕНИЕDISCUSSIONО СТАТЬЕ И.Л. ГУФЕЛЬДА «ГЕОЛОГИЧЕСКИЕ СЛЕДСТВИЯ АМОРФИЗАЦИИ ЛИТОСФЕРЫ И ВЕРХНЕЙ МАНТИИ, ВЫЗВАННЫЕ ВОДОРОДНОЙ ДЕГАЗАЦИЕЙ»ON THE ARTICLE «GEOLOGICAL CONSEQUENCES OF AMORPHIZATION OF THE LITHOSPHERE AND UPPER MANTLE STRUCTURES CAUSED BY HYDROGEN DEGASSING» BY I. L. GUFELDНиколаевАлексей ВсеволодовичNikolaevAlexey V.

докт. физ.мат. наук, профессор, член-корреспондент РАН, председатель Российского экспертного совета по прогнозу землетрясений и оценке сейсмической опасности, зав. лабораторией экспериментальной геофизики,

123995, Москва, ГСП5, ул. Большая Грузинская, 101

Doctor of Physics and Mathematics, Corresponding Member of RAS, Chairman of the Russian Expert Council for Earthquake Prediction and Seismic Hazard Assessment, Head of Laboratory of Experimental Geophysics,

101 Bolshaya Gruzinskaya street, Moscow 123995

nikavs@ifz.ruИнститут физики Земли им. О.Ю. Шмидта РАНРоссияThe Schmidt Institute of Physics of the Earth RASRussian Federation20120210201534437439Copyright © Николаев А.В., 20152015Николаев А.В.Nikolaev A.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/175

В комментарии рассматриваются возможные направления дальнейших исследований по комплексу вопросов, возникающих при анализе процессов взаимодействия восходящих водородных потоков с твердой фазой литосферы и верхней мантии.

The commentary discusses possible directions for further research on the complex of issues arising in the analysis of the interaction of ascending hydrogen flows with the solid phase of the lithosphere and upper mantle.

аморфизация литосферы и верхней мантииводородная дегазациясейсмический процессamorphization of the lithosphere and upper mantlehydrogen degassingseismic processReferencesGufeld I.L., 2012. Geological consequences of amorphization of the lithosphere and upper mantle structures caused by hydrogen degassing. Geodynamics & Tectonophysics 3 (4), 417–435. http://dx.doi.org/10.5800/GT2012340083.Gufeld I.L., 2012. Geological consequences of amorphization of the lithosphere and upper mantle structures caused by hydrogen degassing. Geodynamics & Tectonophysics 3 (4), 417–435. http://dx.doi.org/10.5800/GT2012340083.Gufeld I.L., Matveeva M.I., Novoselov O.N., 2011. Why we cannot predict strong earthquakes in the Earth’s crust. Geodynamics & Tectonophysics 2 (4), 378–415. http://dx.doi.org/10.5800/GT2011240051.Gufeld I.L., Matveeva M.I., Novoselov O.N., 2011. Why we cannot predict strong earthquakes in the Earth’s crust. Geodynamics & Tectonophysics 2 (4), 378–415. http://dx.doi.org/10.5800/GT2011240051.Letnikov F.A., 2001. Ultradeep fluid systems of the Earth and problems of ore formation. Geology of Ore Deposits 43 (4), 259–273.Letnikov F.A., 2001. Ultradeep fluid systems of the Earth and problems of ore formation. Geology of Ore Deposits 43 (4), 259–273.Letnikov F.A., 2006. Fluids in endogenic processes and problems of metallogeny. Russian Geology and Geophysics 47 (12), 1271–1281.Letnikov F.A., 2006. Fluids in endogenic processes and problems of metallogeny. Russian Geology and Geophysics 47 (12), 1271–1281.

The authors declare that there are no conflicts of interest present.