Orientation of an Epidote with a Unique Crystal Habit in a Quartz-Schist from Besshi
廣島大學地學研究報告 Issue 14
Page 233-238
published_at 1965-02-22
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この文献の参照には次のURLをご利用ください : https://doi.org/10.15027/52852
| File | |
| Title ( eng ) |
Orientation of an Epidote with a Unique Crystal Habit in a Quartz-Schist from Besshi
|
| Creator |
KOJIMA George
HIDE Kei
|
| Source Title |
廣島大學地學研究報告
Geological report of the Hiroshima University
|
| Issue | 14 |
| Start Page | 233 |
| End Page | 238 |
| Abstract |
Epidote crystals characterized by the development of the crystallographic plane (102) have been found in a quartz-schist from Besshi, Ehime Pref. The crystallographic axis b of the epidote coincides with fabric axis b of the rock, and the plane (102) is oriented parallel to the fabric plane (ab).
|
| Descriptions |
今村外治教授退官記念特集号
|
| Language |
eng
|
| Resource Type | departmental bulletin paper |
| Publisher |
廣島大學理學部地學教室
|
| Date of Issued | 1965-02-22 |
| Publish Type | Version of Record |
| Access Rights | open access |
| Source Identifier |
[ISSN] 0073-2303
[NCID] AN00213676
|
