Thermal and impact history of the H chondrite parent asteroid during metamorphism: Constraints from metallic Fe–Ni

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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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ORIGIN AND THERMAL HISTORY OF FeNi - METAL IN PRIMITIVE CHONDRITES

M. I. Petaev, A. Meibom, C. Perron, and B. Zanda, Dept. of the Geophysical Sciences, University of Chicago (5734 S. Ellis Ave., Chicago, IL 60637 USA; [email protected]), Dept. of Earth and Planetary Sciences, Harvard University (20 Oxford St., Cambridge, MA 02138 USA; [email protected]), Dept. of Geological and Environmental Sciences, Stanford University (Building 320, Lomita Mall,...

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ژورنال

عنوان ژورنال: Geochimica et Cosmochimica Acta

سال: 2014

ISSN: 0016-7037

DOI: 10.1016/j.gca.2014.03.038