Petrography, shock history, chemical composition and noble gas content of the lunar meteorites Yamato-82192 and -82193

• Main Authors: Bischoff,A., Palme,H., Weber,H.W., Stoffler,D., Braun,O., Spettel,B., Begemann,F., Wanke,H., Ostertag,R.
• Format: Report
• Language: English
• Published: Institute fur Planetologie/Max-Planck-Institute fur Chemie/Max-Planck-Institute fur Chemie/Institute fur Planetologie/Max-Planck-Institute fur Chemie/Max-Planck-Institute fur Chemie/Max-Planck-Institute fur Chemie/Max-Planck-Institute fur Chemie/Institute fur Planetologie 1987
• Subjects: Antarctic; The Antarctic; Yamato; Antarc*; Memoirs of National Institute of Polar Research; Polar Research
• Online Access: https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2118; http://id.nii.ac.jp/1291/00002118/; https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2118&item_no=1&attribute_id=18&file_no=1

The Antarctic meteorites Yamato-82192 and -82193 are lunar polymict shock-lithified fragmental breccias with a minor regolith component. They are probably paired. The breccias are composed of a great variety of lithic and mineral fragments embedded in a fine-grained, densely compacted clastic matrix...