THE EVIDENCE FOR A MISCIBILITY GAP IN THE FE3O4-ZNFE2O4 SYSTEM - A REVIEW

被引：9
作者：
GRAYDON, JW
KIRK, DW
机构：
来源：
METALLURGICAL TRANSACTIONS B-PROCESS METALLURGY | 1988年 / 19卷 / 06期
关键词：
D O I：
10.1007/BF02651414
中图分类号：
TF [冶金工业];
学科分类号：
0806 ;
摘要：
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页码：919 / 925
页数：7
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共 19 条
[1]  
[Anonymous], 1959, FERRITES
[2]  
BENNER RL, 1966, RI6754 BUR MIN
[3]  
Burke E. A. J., 1972, LITHOS, V5, P69
[4]  
DOBSON DC, 1970, J PHYS CHEM SOLIDS, V31, P219
[5]   THERMODYNAMIC PROPERTIES AND CATION DISTRIBUTION OF THE ZNFE2O4-FE3O4 SPINEL SOLID-SOLUTIONS AT 900-DEGREES-C [J].
FITZNER, K .
THERMOCHIMICA ACTA, 1979, 31 (02) :227-236
[6]   THE MECHANISM OF FERRITE FORMATION FROM IRON SULFIDES DURING ZINC ROASTING [J].
GRAYDON, JW ;
KIRK, DW .
METALLURGICAL TRANSACTIONS B-PROCESS METALLURGY, 1988, 19 (05) :777-785
[7]   SYSTEMATICS OF THE SPINEL STRUCTURE TYPE [J].
HILL, RJ ;
CRAIG, JR ;
GIBBS, GV .
PHYSICS AND CHEMISTRY OF MINERALS, 1979, 4 (04) :317-339
[8]  
Katayama I., 1977, Transactions of the Japan Institute of Metals, V18, P743
[9]  
LINDSLEY DH, 1976, MINERALOGICAL SOC AM, V3, pL1
[10]  
MINYATA N, 1961, J PHYS SOC JPN, V16, P1291
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