Diopside in chondrules of Yamato-691 (EH3)
Diopside in the chondrules in Y-691 (EH3), most of which include enstatite as phenocrysts, occurs in three different modes; (1) diopside rimming some of the enstatite crystals, (2) single crystals as phenocrysts of the chondrules, and (3) single crystals of diopside enriched in aluminum in one chond...
Full description
Bibliographic Details
Main Authors: |
Masao Kitamura,
Seiko Watanabe,
Hiroshi Isobe,
Nobuo Morimoto |
Format: | Report
|
Language: | English |
Published: |
Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University
1987
|
Subjects: |
|
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2125
http://id.nii.ac.jp/1291/00002125/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2125&item_no=1&attribute_id=18&file_no=1
|