DOES THE WHOLE OF THE EARTHS CORE CONVECT

被引:157
作者
WHALER, KA
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10.1038/287528a0
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
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07 ; 0710 ; 09 ;
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页码:528 / 530
页数:3
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[2]   STRENGTH OF ELECTRIC CURRENTS AND ZONAL MAGNETIC-FIELDS AT THE TOP OF THE EARTHS CORE - METHODOLOGY AND PRELIMINARY ESTIMATES [J].
BENTON, ER ;
MUTH, LA .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1979, 20 (2-4) :127-133
[3]  
BENTON ER, PHYS EARTH PLANET IN
[4]   PRESSURE-DEPENDENCE OF THERMODYNAMICAL GRUNEISEN PARAMETER OF FLUIDS [J].
BOEHLER, R ;
KENNEDY, GC .
JOURNAL OF APPLIED PHYSICS, 1977, 48 (10) :4183-4186
[5]   ADIABATIC GRADIENT AND MELTING POINT GRADIENT IN CORE OF EARTH [J].
HIGGINS, G ;
KENNEDY, GC .
JOURNAL OF GEOPHYSICAL RESEARCH, 1971, 76 (08) :1870-&
[6]   OBSERVATIONAL CONSTRAINTS ON THE CHEMICAL AND THERMAL STRUCTURE OF THE EARTHS DEEP INTERIOR [J].
MASTERS, G .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1979, 57 (02) :507-534
[7]   ON ANALYSIS OF SECULAR VARIATION .1. A HYDROMAGNETIC CONSTRAINT - THEORY [J].
ROBERTS, PH ;
SCOTT, S .
JOURNAL OF GEOMAGNETISM AND GEOELECTRICITY, 1965, 17 (02) :137-&
[8]  
WHALER KA, GEOPHYS JR ASTR SOC
[9]  
ZMUDA AJ, 1971, IAGA28 B