SUR L'HYPERITE D'ARVIEU (AVEYRON).BERGERON J.1887; C.R. ACAD. SCI.-FR.SER.D; FRA; 1887, VOL. 105, P. 247 A 250Miscellaneous

THE OCCURRENCE OF OLIVINE HYPERITE AT OEDEGARDENS VERK, BAMBLE, SOUTH NORWAY, BY M. GLAVERIS.GRIFFIN WL; HEIER KS.1971; NORSK GEOL. T.; NOR; 1971, VOL. 51, NUM. 0001, P. 89 A 91Miscellaneous

Dilational behaviour of crushed stoneSTEENFLET, J.S; FOGED, N.International congress International Association of Engineering Geology. 1994, pp 3357-3364Conference Paper

THE RELATIONSHIP BETWEEN SOME HYPERITES, GRANITES AND GNEISSES IN SOUTHERN VAERMLAND = RELATIONS ENTRE LES HYPERITES, GRANITES ET GNEISSES AU SUD DU VAERMLANDMALMSTROEM L.1981; SVERIGES GEOLOGISKA UNDERSOEKNING. SERIE C: AVHANDLINGAR OCH UPPSATSER; ISSN 0370-9930; SWE; DA. 1981; VOL. 75; NO 781; PP. 24-30; BIBL. 13 REF.; 1 TAB. ; ESQUISSE/ILL./TABL.Article

THE EARLY MAJOR STRUCTURE AND PETROLOGY OF ROCKS IN THE BAMBLE SERIES, SONDELED-SANDNESFJORD, AUST-AGDERSTARMER IC.1976; NORGES GEOL. UNDERSOEK.; NOR; DA. 1976; NO 327; PP. 77-96; BIBL. 18 REF.; 6 ILL.Article

Volume effect of a gabbro-amphibolite transition = Effet du volume d'une transition gabbro-amphiboliteZECK, H. P; OTTESEN, C; TOFT, J et al.Chemical geology. 1988, Vol 67, Num 1-2, pp 141-153, issn 0009-2541Article