On the thermodynamics of meteorites and parent bodies III. basaltic achondrites in an increasing SIO2 sequence and comparison of the role of diogenites and komatiites in planetary evolution /
After chondritic thermal metamorphism the thermal evolution of a primitive achondritic mineral assemblage continued by partial melting and outflow of the metal-sulfide components and of the low melting point basaltic components. Metal-sulfide assemblage migrated toward the center, basalt migrated to...
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Main Authors: |
Bérczi Szaniszló Holba Ágnes Lukács Béla |
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Format: | Article |
Published: |
Szegedi Egyetem Ásványtani, Geokémiai és Kőzettani Tanszéke
Szeged
2000
|
Series: | Acta mineralogica-petrographica
41 |
Kulcsszavak: | Kőzettan - előadáskivonat, Ásványtan - előadáskivonat, Földtan - előadáskivonat |
Subjects: | |
Online Access: | http://acta.bibl.u-szeged.hu/24900 |
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