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PRIZNAKI UDARNOGO METAMORFIZMA V METEORITE KAALI = INDICES DE METAMORPHISME DE CHOC DANS LA METEORITE KAALISEMENENKO VP; SAMOJLOVICH LG; KOZLOV IS et al.1982; METEORITIKA; ISSN 0369-2507; SUN; DA. 1982; NO 41; PP. 96-100; BIBL. 16 REF.; 2 TAB. ; TABL.Article

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Degassing of H₂O and noble gases on impact shockAZUMA, S.-I; HIYAGON, H; HANYU, T et al.International geological congress. 1992, p.650Conference Paper

Velocity and spin distribution of fragments from impact disruptionNAKAMURA, A; FUJIWARA, A.International geological congress. 1992, p.649Conference Paper

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Features of shock heating in the matrix of the Gujargaon MeteoriteSEN GUPTA, P.R.Visesa Prakasana - Bharatiya Bhuvaijñanika Sarveksana. 1991, Num 16, pp 51-52, issn 0254-0436Article

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EKSPERIMENTAL'NOYE MODELIROVANIYE UDARNOGO METAMORFIZMA MINERALOV = EXPERIMENTAL MODELING OF SHOCK METAMORPHISM IN MINERALS = UN MODELE EXPERIMENTAL DE METAMORPHISME DE CHOC DANS LES MINERAUXBADYUKOV DD; MARAKUSHEVA AA ED.1981; IMPAKTITY; SUN; MOSCOW:IZD. MOSK. UNIV.; DA. 1981; PP. 20-34; 7 TAB. ; ILL.Book Chapter

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TETRATAENITE AND THE ORIGIN OF MAGMATIC METEORITES = LA TETRATAENITE ET L'ORIGINE DES METEORITES MAGNETIQUESALBERTSEN JF; ROY POULSEN NO; VISTISEN L et al.1981; METEORITICS; ISSN 0026-1114; USA; DA. 1981; VOL. 16; NO 4; PP. 288Conference Paper

PLANARNYYE DEFORMATSII V MINERALAKH KAK INDIKATOR UDARNOGO METAMORFIZMA = PLANAR DEFORMATION IN MINERALS AS AN INDICATOR OF SHOCK METAMORPHISM = LA DEFORMATION PLANAIRE DANS LES MINERAUXKAROTAYEVA NN; SAZONOVA LV; MARAKUSHEVA AA ED et al.1981; IMPAKTITY; SUN; MOSCOW:IZD. MOSK. UNIV.; DA. 1981; PP. 35-55; 8 TAB. ; ILL.Book Chapter