Reclassification and thermal history of Trenzano chondrite

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Thermal constraints on the early history of the H-chondrite parent body reconsidered

Reconstructions of the early thermal history of the H-chondrite parent body have focused on two competing hypotheses. The first posits an undisturbed thermal evolution in which the degree of metamorphism increases with depth, yielding an “onion-shell” structure. The second posits an early fragmentation–reassembly event that interrupted this orderly cooling process. Here, we test these hypothese...

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ژورنال

عنوان ژورنال: Meteoritics & Planetary Science

سال: 2007

ISSN: 1086-9379,1945-5100

DOI: 10.1111/j.1945-5100.2007.tb01007.x