EXPERIMENTAL INVESTIGATION OF METAMORPHISM OF SILICEOUS DOLOMITES .1. EQUILIBRIUM DATA OF REACTION - 3 DOLOMITE+4QUARTZ+1H2O LESS THAN GREATER THAN TALC+3CALCITE+3CO2 DETERMINED FOR TOTAL PRESSURES OF 1000, 3000, AND 5000 BARS

被引:29
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METZ, P
PUHAN, D
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10.1007/BF00390079
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P3 [地球物理学]; P59 [地球化学];
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0708 ; 070902 ;
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共 33 条
[1]  
ALTHAUS E, 1969, NEUES JB MINER ABH, V111, P74
[2]   Progressive metamorphism of siliceous limestone and dolomite [J].
Bowen, NL .
JOURNAL OF GEOLOGY, 1940, 48 (03) :225-274
[3]  
COOPER JR, 1957, GEOL SOC AM BULL, V68, P577
[4]   On contact phenomena between gneiss and limestone in western Massachusetts [J].
Eskola, P .
JOURNAL OF GEOLOGY, 1922, 30 (04) :265-294
[5]  
ESKOLA P, 1939, BARTH CORRENS ESKOLA
[6]   STABILITY RELATIONS OF THE FERRUGINOUS BIOTITE, ANNITE [J].
EUGSTER, HP ;
WONES, DR .
JOURNAL OF PETROLOGY, 1962, 3 (01) :82-&
[7]  
EUGSTER HP, 1967, RESEARCHES GEOCHEMIS, V2
[8]   EXPERIMENTAL CONTROL OF OXYGEN FUGACITIES BY GRAPHITE-GAS EQUILIBRIUMS [J].
FRENCH, BM ;
EUGSTER, HP .
JOURNAL OF GEOPHYSICAL RESEARCH, 1965, 70 (06) :1529-&
[10]  
GANGULY H, 1968, J PETROL, V9, P444