Reduced and unstratified crust in CV chondrite parent body

The Tagish Lake Chondrite and the Interstellar Parent Body

Magnetic evidence for a partially differentiated carbonaceous chondrite parent body

Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139; Berkeley Geochronology Center, Berkeley, CA 94709; Department of Earth and Planetary Science, University of California, Berkeley, CA 94720; Department of Earth and Planetary Sciences, American Museum of Natural History, New York, NY 10024; and Centre Européen de Recherche et d’E...

Evidence for Internally Generated Magnetic Fields on the Cv Chondrite Parent Planetesimal

Introduction: The aggregational texture and bulk chemical composition of chondrites demonstrate that they are not the products of planetary melting proceses. As a result, chondrites have traditionally been thought to samples bodies that have not undergone large-scale differentiation [1]. However, it has long been known that CV and other carbonaceous chondrites carry a stable natural remanent ma...

Mineralogy and Petrography of Mil 090001, a Highly Altered Cv Chondrite from the Reduced Sub-group

Joint Thermal and Collisional Modeling of the H-chondrite Parent Body

Grimm, W.F. Bottke, D. Durda, B. Enke, E.R.D. Scott, E. Asphaug, D. Richardson. Space Studies Department, Southwest Research Institute, 1050 Walnut St. #400, Boulder, CO 80302, [email protected]. Hawaii Institute of Geophysics and Planetology, University of Hawaii, Manoa. Earth Sciences Department, University of California, Santa Cruz. Department of Astronomy, University of Maryland, Colle...