On the thermodynamics of meteorites and parent bodies II. from chondrites through the primitive achondrite verities (stage A and stage B) to the basaltic achondrites /
We study the degrees of thermal evolution over chondritic stages: via primitive achondritic (stage A) stage of acapulcoites, lodranites, winonaites and IAB iron silicate inclusions, through the (stage B) primitive achondrites of ureilites and some lodranites till the basaltic achondrites. We discuss...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1999
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| Sorozat: | Acta mineralogica-petrographica
40 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24887 |
| Tartalmi kivonat: | We study the degrees of thermal evolution over chondritic stages: via primitive achondritic (stage A) stage of acapulcoites, lodranites, winonaites and IAB iron silicate inclusions, through the (stage B) primitive achondrites of ureilites and some lodranites till the basaltic achondrites. We discuss the utility of notion of E, H, L and LL primitive achondrites, too. In this paper we are continuing our previous work of evolutionally arranging the stony meteorites. |
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| Terjedelem/Fizikai jellemzők: | 175-198 |
| ISSN: | 0365-8066 |