HIGH MAGNESIA LIQUIDS AS THE PARENTAL MAGMA FOR OCEAN-FLOOR BASALTS

被引:127
作者
ELTHON, D [1 ]
机构
[1] COLUMBIA UNIV,DEPT GEOL SCI,NEW YORK,NY 10027
关键词
D O I
10.1038/278514a0
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];
学科分类号
07 ; 0710 ; 09 ;
摘要
The primary melt segregating from the upper mantle beneath an oceanic ridge is shown to contain ~18% MgO. Whereas these primary liquids are capable of generating the petrological features of the oceanic crust, this is not possible for tholeiitic basalts with 9-11% MgO which are highly fractionated. Compositions of liquids ranging from primary melts to high calcium picrites from the Tortuga ophiolite complex, Chile, are reported. © 1979 Nature Publishing Group.
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页码:514 / 518
页数:5
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