SCANNING CALORIMETRIC DETERMINATIONS OF THE HEAT CONTENTS OF DIOPSIDE-RICH SYSTEMS DURING MELTING AND CRYSTALLIZATION

被引:8
作者
DEYOREO, JJ [1 ]
LANGE, RA [1 ]
NAVROTSKY, A [1 ]
机构
[1] PRINCETON UNIV,DEPT GEOL SCI,PRINCETON,NJ 08544
关键词
D O I
10.1016/0016-7037(95)00166-W
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The results of scanning calorimetric measurements on crystalline albite, diopside, diopside-anorthite, and diopside-wollastonite-enstatite are reported in the temperature range of 1300 K to 1775 K. The results for albite agree with those obtained previously using a drop-calorimetric technique and confirm that melting takes place during a 300 K temperature interval starting near the accepted equilibrium melting point of 1373 K. The heat content, H(T), of anorthite-diopside mixtures is calculated numerically based on existing thermodynamic data. The results are compared to measurements on a mechanical mixture of 10 mol% anorthite-90 mol% diopside containing 3% of second phase impurities. Due to the presence of these impurities, the onset of premelting or melting occurs at 150 K below the An-Di eutectic and the heat of fusion at the liquidus (1665 K) is 114 +/- 6 kJ/mol, which is 6% less than calculated for the pure mixture. Measurements of H(T) on a sample of 13 mol% wollastonite-83 mol% diopside are also presented. The measured heat of fusion at 1665 K is 125 +/- 7 kJ/mol, in excellent agreement with the value of 124.8 kJ/mol calculate from existing thermodynamic data. Our data place an upper limit of 7 kJ/mol on the heat of mixing in this system at 1665 K.
引用
收藏
页码:2701 / 2707
页数:7
相关论文
共 24 条
[1]  
ADAMKOVICOVA K, 1980, SILIKATY, V24, P193
[2]   NUCLEATION, CRYSTAL-GROWTH AND THE THERMAL REGIME OF COOLING MAGMAS [J].
BRANDEIS, G ;
JAUPART, C ;
ALLEGRE, CJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB12) :161-177
[3]  
GAUNEESCARD M, 1974, CAN METALL QUART, V13, P335
[4]  
Ghiorso M.S., 1991, PROGR METAMORPHIC MA, P387
[5]   THERMAL DEVELOPMENT OF LOW-PRESSURE METAMORPHIC BELTS - RESULTS FROM TWO-DIMENSIONAL NUMERICAL-MODELS [J].
HANSON, RB ;
BARTON, MD .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1989, 94 (B8) :10363-10377
[6]   THE GENERATION OF GRANITIC MAGMAS BY INTRUSION OF BASALT INTO CONTINENTAL-CRUST [J].
HUPPERT, HE ;
SPARKS, RSJ .
JOURNAL OF PETROLOGY, 1988, 29 (03) :599-624
[7]   HIGH-TEMPERATURE DEFORMATION OF DIOPSIDE SINGLE-CRYSTAL .2. TRANSMISSION ELECTRON-MICROSCOPY INVESTIGATION OF THE DEFECT MICROSTRUCTURES [J].
INGRIN, J ;
DOUKHAN, N ;
DOUKHAN, JC .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1991, 96 (B9) :14287-14297
[8]  
KIRKPATRICK RJ, 1981, AM MINERAL, V66, P223
[9]  
LANGE RA, 1991, AM MINERAL, V76, P904
[10]   THE EXTRACTION OF MAGMA FROM THE CRUST AND MANTLE [J].
MCKENZIE, D .
EARTH AND PLANETARY SCIENCE LETTERS, 1985, 74 (01) :81-91