Bérczi, Szaniszló

Gál-Sólymos, Kamilla

Holba, Ágnes

Lukács, Béla

Martinás, Katalin

English

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

Bérczi Szaniszló

Gál-Sólymos Kamilla

Holba Ágnes

Lukács Béla

Martinás Katalin

University of Szeged

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

http://acta.bibl.u-szeged.hu/24887/1/mineralogica_040_175-198.pdf

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

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University of Szeged