A Preliminary Mineralogical Examination of the Yamato-74 Achondrites
P(論文) Seven diogenites, two eucritic polymict breccias and one pallasite have been identified in the Yamato-74 meteorites by the electron microprobe and single crystal X-ray diffraction techniques. The texture of Yamato-74010,-74011,-74013,-74037,-74097,-74136 and -74648 is unlike those of the other...
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ftnipr:oai:nipr.repo.nii.ac.jp:00000886 2024-09-09T19:51:58+00:00 A Preliminary Mineralogical Examination of the Yamato-74 Achondrites Takeda, Hiroshi Miyamoto, Masamichi Yanai, Keizo Haramura, Hiroshi 1978-02 application/pdf https://nipr.repo.nii.ac.jp/record/886/files/KJ00000011859.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 8 170 184 AA00733561 https://nipr.repo.nii.ac.jp/record/886/files/KJ00000011859.pdf 1978 ftnipr 2024-06-17T04:04:30Z P(論文) Seven diogenites, two eucritic polymict breccias and one pallasite have been identified in the Yamato-74 meteorites by the electron microprobe and single crystal X-ray diffraction techniques. The texture of Yamato-74010,-74011,-74013,-74037,-74097,-74136 and -74648 is unlike those of the other diogenites. It is not brecciated and texturally the pyroxene seems to have recrystallized to a granoblastic texture with small change in mineral composition. The chemical composition of the orthopyroxenes in these diogenites falls in the range (Ca)_<1.9> (Mg)_<75.1> (Fe)_<23.0> to (Ca)_<3.0> (Mg)_<71.0> (Fe)_<26.0>. The chemistry and textures of these diogenites are the same as those of the Yamato-6902 (b) diogenite previously reported. These Yamato diogenites may represent fragments of the same fall. Yamato-74159 is a polymict breccia which contains mineral and lithic clasts common to eucrites. The Yamato-74450 eucrite shows a variolitic texture, indicating a rapid solidification near the surface of its parent body. A brecciated part containing a pigeonite crystal with augite lamellae is also found in small amounts. The pyroxene trends of Yamato-74450 resemble those of the Pasamonte eucrite. The Yamato-74044 pallasite is the only stony-iron meteorite among the Yamato collection. A preliminary examination of the Yamato-75 meteorites identified one iron-rich diogenite and two eucritic polymict breccias. Yamato-75032 is the most Fe-rich of any known diogenite. 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) Seven diogenites, two eucritic polymict breccias and one pallasite have been identified in the Yamato-74 meteorites by the electron microprobe and single crystal X-ray diffraction techniques. The texture of Yamato-74010,-74011,-74013,-74037,-74097,-74136 and -74648 is unlike those of the other diogenites. It is not brecciated and texturally the pyroxene seems to have recrystallized to a granoblastic texture with small change in mineral composition. The chemical composition of the orthopyroxenes in these diogenites falls in the range (Ca)_<1.9> (Mg)_<75.1> (Fe)_<23.0> to (Ca)_<3.0> (Mg)_<71.0> (Fe)_<26.0>. The chemistry and textures of these diogenites are the same as those of the Yamato-6902 (b) diogenite previously reported. These Yamato diogenites may represent fragments of the same fall. Yamato-74159 is a polymict breccia which contains mineral and lithic clasts common to eucrites. The Yamato-74450 eucrite shows a variolitic texture, indicating a rapid solidification near the surface of its parent body. A brecciated part containing a pigeonite crystal with augite lamellae is also found in small amounts. The pyroxene trends of Yamato-74450 resemble those of the Pasamonte eucrite. The Yamato-74044 pallasite is the only stony-iron meteorite among the Yamato collection. A preliminary examination of the Yamato-75 meteorites identified one iron-rich diogenite and two eucritic polymict breccias. Yamato-75032 is the most Fe-rich of any known diogenite. departmental bulletin paper |
author |
Takeda, Hiroshi Miyamoto, Masamichi Yanai, Keizo Haramura, Hiroshi |
spellingShingle |
Takeda, Hiroshi Miyamoto, Masamichi Yanai, Keizo Haramura, Hiroshi A Preliminary Mineralogical Examination of the Yamato-74 Achondrites |
author_facet |
Takeda, Hiroshi Miyamoto, Masamichi Yanai, Keizo Haramura, Hiroshi |
author_sort |
Takeda, Hiroshi |
title |
A Preliminary Mineralogical Examination of the Yamato-74 Achondrites |
title_short |
A Preliminary Mineralogical Examination of the Yamato-74 Achondrites |
title_full |
A Preliminary Mineralogical Examination of the Yamato-74 Achondrites |
title_fullStr |
A Preliminary Mineralogical Examination of the Yamato-74 Achondrites |
title_full_unstemmed |
A Preliminary Mineralogical Examination of the Yamato-74 Achondrites |
title_sort |
preliminary mineralogical examination of the yamato-74 achondrites |
publishDate |
1978 |
url |
https://nipr.repo.nii.ac.jp/record/886/files/KJ00000011859.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 8 170 184 AA00733561 https://nipr.repo.nii.ac.jp/record/886/files/KJ00000011859.pdf |
_version_ |
1809921314709831680 |