Pascal and Francis Bibliographic Databases

Help

Search results

Your search

kw.\*:("600-1100-C")

Results 1 to 4 of 4

  • Page / 1

Export

Selection :

  • and

DETERMINATION OF THE COESITE-STISHOVITE TRANSITION BY IN SITU X-RAY MEASUREMENT.AKIMOTO S; YAGI T.sdIN: INT. UNION GEOD. GEOPHYS. GEN. ASSEM. 16; GRENOBLE; 1975; PARIS IMPR. SCHIFFER; RESUME,1975, P. 12Miscellaneous

DIRECT DETERMINATION OF THE QUARTZ-COESITE TRANSITION BY IN SITU X-RAY MEASUREMENTS.BOEHLER R; ARNDT J.1974; CONTRIB. MINERAL. PETROL.; DEU; 1974, VOL. 48, NUM. 0002, P. 149 A 152Serial Issue

THE MISCIBILITY GAP BETWEEN RHODONITE AND BUSTAMITE ALONG THE JOIN MNSIO3-CA0.60MN0.40SIO3 = LACUNE DE MISCIBILITE ENTRE LA RHODONITE ET LA BUSTAMITE LE LONG DU JOINT MNSIO3-CA0,60)MN0,40)SIO3ABRECHT J; PETERS TJ.1980; CONTRIB. MINERAL. PETROL.; ISSN 0010-7999; DEU; DA. 1980; VOL. 74; NO 3; PP. 261-269; BIBL. 1 P.; 21 ANAL.; 2 TAB. ; ILL./ANAL.Article

THE ROLE OF SPHENE AS AN ACCESSORY PHASE IN THE HIGH-PRESSURE PARTIAL MELTING OF HYDROUS MAFIC COMPOSITIONSHELLMAN PL; GREEN TH.1979; EARTH PLANET. SCI. LETTERS; NLD; DA. 1979; VOL. 42; NO 2; PP. 191-201; BIBL. 45 REF.; 4 ILL.Article

  • Page / 1