Petrological Studies on Yamato-74354, -74190, -74362, -74646 and -74115 Chondrites
P(論文) Petrological description has been done on five different Yamato-74354 (L6), -74362 (L6), -74190 (L6), -74646 (LL6) and -74115 (H5) chondrites. Detailed microprobe analyses of the constituent minerals and chondrules indicate that these chondrites consist of homogeneous silicate minerals and rem...
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ftnipr:oai:nipr.repo.nii.ac.jp:00001045 2024-09-09T19:51:59+00:00 Petrological Studies on Yamato-74354, -74190, -74362, -74646 and -74115 Chondrites Nagahara, Hiroko 1979-12 application/pdf https://nipr.repo.nii.ac.jp/record/1045/files/KJ00000011589.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 15 77 109 AA00733561 https://nipr.repo.nii.ac.jp/record/1045/files/KJ00000011589.pdf 1979 ftnipr 2024-06-17T04:00:22Z P(論文) Petrological description has been done on five different Yamato-74354 (L6), -74362 (L6), -74190 (L6), -74646 (LL6) and -74115 (H5) chondrites. Detailed microprobe analyses of the constituent minerals and chondrules indicate that these chondrites consist of homogeneous silicate minerals and remarkably heterogeneous Fe-Ni metals. They show various degrees of recrystallization but the equilibrium temperature of olivine, pyroxenes and chromite is about 900℃ and is quite similar among these five chondrites. The degree of recrystallization, therefore, would depend not only on the equilibrium temperature but also largely on the duration of recrystallization. It is also suggested that the bulk chemical composition of chondrules has been hardly affected by thermal metamorphism. departmental bulletin paper Other/Unknown Material Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Yamato ENVELOPE(35.583,35.583,-71.417,-71.417) |
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Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
P(論文) Petrological description has been done on five different Yamato-74354 (L6), -74362 (L6), -74190 (L6), -74646 (LL6) and -74115 (H5) chondrites. Detailed microprobe analyses of the constituent minerals and chondrules indicate that these chondrites consist of homogeneous silicate minerals and remarkably heterogeneous Fe-Ni metals. They show various degrees of recrystallization but the equilibrium temperature of olivine, pyroxenes and chromite is about 900℃ and is quite similar among these five chondrites. The degree of recrystallization, therefore, would depend not only on the equilibrium temperature but also largely on the duration of recrystallization. It is also suggested that the bulk chemical composition of chondrules has been hardly affected by thermal metamorphism. departmental bulletin paper |
author |
Nagahara, Hiroko |
spellingShingle |
Nagahara, Hiroko Petrological Studies on Yamato-74354, -74190, -74362, -74646 and -74115 Chondrites |
author_facet |
Nagahara, Hiroko |
author_sort |
Nagahara, Hiroko |
title |
Petrological Studies on Yamato-74354, -74190, -74362, -74646 and -74115 Chondrites |
title_short |
Petrological Studies on Yamato-74354, -74190, -74362, -74646 and -74115 Chondrites |
title_full |
Petrological Studies on Yamato-74354, -74190, -74362, -74646 and -74115 Chondrites |
title_fullStr |
Petrological Studies on Yamato-74354, -74190, -74362, -74646 and -74115 Chondrites |
title_full_unstemmed |
Petrological Studies on Yamato-74354, -74190, -74362, -74646 and -74115 Chondrites |
title_sort |
petrological studies on yamato-74354, -74190, -74362, -74646 and -74115 chondrites |
publishDate |
1979 |
url |
https://nipr.repo.nii.ac.jp/record/1045/files/KJ00000011589.pdf |
long_lat |
ENVELOPE(35.583,35.583,-71.417,-71.417) |
geographic |
Yamato |
geographic_facet |
Yamato |
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 15 77 109 AA00733561 https://nipr.repo.nii.ac.jp/record/1045/files/KJ00000011589.pdf |
_version_ |
1809921350128631808 |