The paradox between low shock-stage and evidence for compaction in CM carbonaceous chondrites explained by multiple low-intensity impacts (2015)
Attributed to:
Reconstructing thermal and fluid alteration histories of planetary materials
funded by
STFC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.gca.2014.09.014
Publication URI: http://dx.doi.org/10.1016/j.gca.2014.09.014
Type: Journal Article/Review
Parent Publication: Geochimica et Cosmochimica Acta