離溶により生じた単斜シソ輝石母体の結晶構造について

島根大学理学部紀要 Volume 19 Page 151-157 published_at 1985-12-25
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Title
離溶により生じた単斜シソ輝石母体の結晶構造について
Title
On the Structure of Clinohypersthene Derived as a Host Phase from Parental Pigeonite by Exsolution
Title Transcription
リヨウ ニヨリ ショウジタ タンシャ シソキセキ ボタイ ノ ケッショウ コウゾウ ニツイテ
Creator
Yamaguchi Yoshiaki
Tomita Katsutoshi
Source Title
島根大学理学部紀要
Memoirs of the Faculty of Science, Shimane University
Volume 19
Start Page 151
End Page 157
Journal Identifire
ISSN 03879925
Descriptions
Structure refinement was made for a clinohypersthene C_<.02> Mg_<.51> Fe_<.47> Si_20_6, derived as a host phase from parental pigeonite by exsolution of augite along the metastable extension of the pigeonite solvus into the stability field of hypersthene. The particular characteristics of the structure are discussed, and compared with those of pigeonite and orthohypersthene. The clinohypersthene shows no indication of anti-phase domain structure on the reflections with (h+k) odd, and has six-fold coordination of oxygen around M2 site. Clino- and orthopyroxenes of hypersthene composition have closely similar atomic parameters. Kinetic factors are expected to be strongly responsible for the metastable extension of the pigeonite solvus.
Language
eng
Resource Type departmental bulletin paper
Publisher
島根大学理学部
The Faculty of Science, Shimane University
Date of Issued 1985-12-25
Access Rights open access
Relation
[NCID] AN00108106