000 01251nab a2200361 1n4500
001 000082139
005 20250722191031.0
008 930303s1982 000 0 eng d
022 _a00167606
041 0 7 _aEng
_2ISO 639-1
084 _aRev 343
100 1 _aWyllie, Peter
_916136
245 1 0 _aSubduction products according to experimental prediction
504 _abibliogr. p. 476
500 _a<Donation ORSTOM>
650 0 4 _aSubduction zone
_916134
650 0 4 _aCro–te océanique
_92090
650 0 4 _aPétrologie
_96859
650 0 4 _aAmphibolite
_915618
650 0 4 _aPeridotite
_913700
650 0 4 _aMagma
_96936
650 0 4 _aAndesite
_915298
650 0 4 _aMagma basique
_916137
650 0 4 _aBasalte
_911948
650 0 4 _aRhyolite
_915165
650 0 4 _aFusion partielle
_915938
650 0 4 _aManteau
_913949
773 0 _tGeological Society of America bulletin
_dBoulder : [s.n.], 1982
_g93(6), 1982, p. 468-476: : ill., graph., rés.(Angl)
711 2 _aRelationships between variations in the subduction of oceanic plates and variations in the magmatic and mineralogic subtances believed to be the products of subduction
_d( Nov. 1979)
_916135
910 _aGSL
_c20150612
_h1025
942 _cANAL
999 _c7994
_d7994