A. Rotman

发表

The Anabar collision system as an element of the Columbia supercontinent: 600 Ma of compression (2.0–1.3 Ga)

O. Rosen, D. Zhuravlev, Z. Spetsius, 2007 .

Syn- and post-eruptive volcanic processes in the Yubileinaya kimberlite pipe, Yakutia, Russia, and implications for the emplacement of South African-style kimberlite pipes

G. V. Kolesnikov, S. Kurszlaukis, I. Mahotkin, 2009 .

Regularities and mechanism of formation of the mantle lithosphere structure beneath the Siberian Craton in comparison with other cratons

T. Ntaflos, R. Mitchell, H. Downes, 2013 .

CLINOPYROXENE GEOTHERMS FOR THE MANTLE COLUMNS BENEATH KIMBERLITE PIPES FROM SIBERIAN CRATON

A. Logvinova, I. Ashchepkov, N. Sobolev, 2003 .

Structure and evolution of the lithospheric mantle beneath Siberian craton, thermobarometric study

A. Logvinova, I. Ashchepkov, N. Pokhilenko, 2010 .

Paleoproterozoic accretion in the Northeast Siberian craton: Isotopic dating of the Anabar collision system

O. Rosen, D. Zhuravlev, Z. Spetsius, 2006 .

Composition and thermal structure of the lithospheric mantle beneath kimberlite pipes from the Catoca cluster, Angola

S. Somov, H. Downes, A. Logvinova, 2012 .

Origin of kimberlites: Evidence from isotopic-geochemical data

I. V. Serov, T. Morikiyo, A. Rotman, 2004 .

Reconstruction of mantle sections beneath Yakutian kimberlite pipes using monomineral thermobarometry

A. Logvinova, I. Ashchepkov, N. Pokhilenko, 2008 .

Peculiarities of diamonds from the commercial deposits of Russia

O. E. Koval’chuk, V. Garanin, A. Rotman, 2011 .