Microstructural evidence for a disequilibrium condensation origin for hibonite‐spinel inclusions in the ALHA 77307 CO 3.0 chondrite-Reference-Cited by-同舟云学术

Microstructural evidence for a disequilibrium condensation origin for hibonite‐spinel inclusions in the ALHA 77307 CO 3.0 chondrite

Published:2015-11-06 Issue:12 Volume:50 Page:2121-2136
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Han Jangmi¹²³,Brearley Adrian J.¹,Keller Lindsay P.³

Affiliation:

1. Department of Earth and Planetary Sciences University of New Mexico Albuquerque New Mexico 87131 USA

2. USRA Lunar and Planetary Institute 3600 Bay Area Houston Texas 77058 USA

3. NASA Johnson Space Center 2101 NASA Parkway Houston Texas 77058 USA

Funder

National Aeronautics and Space Administration

National Science Foundation

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.12563

Reference47 articles.

1. The stability of hibonite, melilite and other aluminous phases in silicate melts: Implications for the origin of hibonite-bearing inclusions from carbonaceous chondrites

2. Organic matter and metamorphic history of CO chondrites

3. DavisA. M.1985.Refractory inclusions in the Ornans C3O chondrite(abstract). 16th Lunar and Planetary Science Conference. p.165.

4. DavisA. M.andHintonR. W.1986.Magnesium and titanium isotopic compositions and trace element chemistry of refractory inclusions in the Ornans carbonaceous chondrite (abstract). 17th Lunar and Planetary Science Conference. p.154.

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