Leonid M. Parfenov
Russian Academy of Sciences
34 Papers
163 Citations
Leonid M. Parfenov is an academic researcher from Russian Academy of Sciences. The author has contributed to research in topics: Terrane & Geodynamics. The author has an hindex of 11, co-authored 34 publications.
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Papers
Circum-North Pacific tectonostratigraphic terrane map
Warren J. Nokleberg,Leonid M. Parfenov,J. W. H. Monger,Boris B. Baranov,Stanislav G. Byalobzhesky,Thomas K. Bundtzen,Tracey D. Feeney,Kazuya Fujita,Steven P. Gordey,Arthur Grantz,Alexander I. Khanchuk,Boris A. Natal'in,L. M. Natapov,Ian O. Norton,William W. Patton,George Plafker,David W. Scholl,Sergei D. Sokolov,Gleb M. Sosunov,David B. Stone,Rowland W. Tabor,Nickolai V. Tsukanov,Tracy L. Vallier,Koji Wakita +23 more
- 01 Jan 1994
Summary of Northeast Asia geodynamics and tectonics
Leonid M. Parfenov,Gombosuren Badarch,Nikolai A. Berzin,Alexander I. Khanchuk,Mikhail I. Kuzmin,Warren J. Nokleberg,Andrei V. Prokopiev,Masatsugu Ogasawara,Hongquan Yan +8 more
TL;DR: A summary of the regional dynamics and tectonics of Northeast Asia as developed for a new summary geodynamics map of the region is presented in this paper, which substantially aids in the understanding of the origin of major rock units, major structures, and contained mineral and fuel resources.
Terranes and Accretionary History of the Transbaikal Orogenic Belts
TL;DR: The Transbaikal orogenic belts are located in southern Siberia and include the Baikal-Patom fold-and-thrust belt, together with the Siberian platform forming the North Asian craton and a collage of terranes to the south of the belt that were accreted to the craton in Late Riphean and Early to Late Paleozoic times.
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Cooperative program helps decipher tectonics of northeastern Russia
TL;DR: Recently obtained paleomagnetic, geochronologic, and seismic data are greatly improving our understanding of the tectonics of northeastern Russia, which lies in an accretionary zone between the stable platforms of the North American and Eurasian plates as mentioned in this paper.
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