Ferropseudobrookite-silica mineral-albite-chondrule in the ALH-77015 chondrite (L3)

P(論文) Ferropseudobrookite-silica mineral-albite-chondrule was found in an unequilibraed (L3) chondrite (ALH-77015). This is the first finding of ferropseudobrookite in chondrite. The ferropseudobrookite exhibits a weakly zonal structure. The stability field of ferropseudobrookite suggests that the c...

Full description

Bibliographic Details
Main Authors: Fujimaki, Hirokazu, Matsu-ura, Mikio, Aoki, Ken-ichiro, Sunagawa, Ichiro
Language:English
Published: 1981
Subjects:
Memoirs of National Institute of Polar Research
Polar Research
Online Access:https://nipr.repo.nii.ac.jp/record/1208/files/KJ00000011734.pdf
id ftnipr:oai:nipr.repo.nii.ac.jp:00001208
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001208 2024-09-09T19:52:00+00:00 Ferropseudobrookite-silica mineral-albite-chondrule in the ALH-77015 chondrite (L3) Fujimaki, Hirokazu Matsu-ura, Mikio Aoki, Ken-ichiro Sunagawa, Ichiro 1981-12 application/pdf https://nipr.repo.nii.ac.jp/record/1208/files/KJ00000011734.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 20 119 123 AA00733561 https://nipr.repo.nii.ac.jp/record/1208/files/KJ00000011734.pdf 1981 ftnipr 2024-06-17T04:00:26Z P(論文) Ferropseudobrookite-silica mineral-albite-chondrule was found in an unequilibraed (L3) chondrite (ALH-77015). This is the first finding of ferropseudobrookite in chondrite. The ferropseudobrookite exhibits a weakly zonal structure. The stability field of ferropseudobrookite suggests that the chondrule should have been quenched at a temperature near 1140±10℃. departmental bulletin paper Other/Unknown Material Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description P(論文) Ferropseudobrookite-silica mineral-albite-chondrule was found in an unequilibraed (L3) chondrite (ALH-77015). This is the first finding of ferropseudobrookite in chondrite. The ferropseudobrookite exhibits a weakly zonal structure. The stability field of ferropseudobrookite suggests that the chondrule should have been quenched at a temperature near 1140±10℃. departmental bulletin paper
author Fujimaki, Hirokazu
Matsu-ura, Mikio
Aoki, Ken-ichiro
Sunagawa, Ichiro
spellingShingle Fujimaki, Hirokazu
Matsu-ura, Mikio
Aoki, Ken-ichiro
Sunagawa, Ichiro
Ferropseudobrookite-silica mineral-albite-chondrule in the ALH-77015 chondrite (L3)
author_facet Fujimaki, Hirokazu
Matsu-ura, Mikio
Aoki, Ken-ichiro
Sunagawa, Ichiro
author_sort Fujimaki, Hirokazu
title Ferropseudobrookite-silica mineral-albite-chondrule in the ALH-77015 chondrite (L3)
title_short Ferropseudobrookite-silica mineral-albite-chondrule in the ALH-77015 chondrite (L3)
title_full Ferropseudobrookite-silica mineral-albite-chondrule in the ALH-77015 chondrite (L3)
title_fullStr Ferropseudobrookite-silica mineral-albite-chondrule in the ALH-77015 chondrite (L3)
title_full_unstemmed Ferropseudobrookite-silica mineral-albite-chondrule in the ALH-77015 chondrite (L3)
title_sort ferropseudobrookite-silica mineral-albite-chondrule in the alh-77015 chondrite (l3)
publishDate 1981
url https://nipr.repo.nii.ac.jp/record/1208/files/KJ00000011734.pdf
genre Memoirs of National Institute of Polar Research
Polar Research
genre_facet Memoirs of National Institute of Polar Research
Polar Research
op_relation Memoirs of National Institute of Polar Research. Special issue
20
119
123
AA00733561
https://nipr.repo.nii.ac.jp/record/1208/files/KJ00000011734.pdf
_version_ 1809921357727662080

Similar Items