Thermal history of ureilite, Pecora Escarpment 82506 deduced from cation distribution and diffusion profile of minerals
PCA82506 is relatively unshocked compared with most ureilites. Large unshocked pigeonite and olivine crystals were studied by means of single crystal X-ray diffraction, analytical TEM, optical microscope and an electronprobe. The chemical compositions of the PCA82506 pigeonites are (Ca)_6(Mg)_<76...
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ftnipr:oai:nipr.repo.nii.ac.jp:00001965 2023-05-15T17:10:59+02:00 Thermal history of ureilite, Pecora Escarpment 82506 deduced from cation distribution and diffusion profile of minerals Toyoda,Hiromi Haga,Nobuhiko Tachikawa,Osamu Takeda,Hiroshi Ishii,Teruaki 1986-07 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1965 http://id.nii.ac.jp/1291/00001965/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1965&item_no=1&attribute_id=18&file_no=1 en eng Mineralogical Institute, Faculty of Sciences, University of Tokyo/Mineralogical Institute, Faculty of Sciences, University of Tokyo/Mineralogical Institute, Faculty of Sciences, University of Tokyo/Mineralogical Institute, Faculty of Sciences, University of Tokyo/Ocean Research Institute, University of Tokyo https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1965 http://id.nii.ac.jp/1291/00001965/ AA00733561 Memoirs of National Institute of Polar Research. Special issue, 41, 206-221(1986-07) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1965&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1986 ftnipr 2022-11-12T19:42:46Z PCA82506 is relatively unshocked compared with most ureilites. Large unshocked pigeonite and olivine crystals were studied by means of single crystal X-ray diffraction, analytical TEM, optical microscope and an electronprobe. The chemical compositions of the PCA82506 pigeonites are (Ca)_6(Mg)_<76>(Fe)_<18>, while the average olivine core composition is (Fa)_<20>. A region about 50 micrometer apart from the olivine rim is reduced by the carbonaceous (C) matrix. From the diffusion profiles of olivine crystals, a cooling rate of 10-15℃/h is estimated by the computer simulation method of MIYAMOTO et al. (Proc. Lunar Planet. Sci. Conf., 16th, Pt. 1,D116,1985). The cell dimensions of the PCA82506 pigeonite determined from 23 reflections are : a, 9.6649(9); b, 8.8719(6); c, 5.2134(5)A; and β, 108.51(6)°. The site occupancy factors are M1 (Mg 0.064,Fe 0.936) and M2 (Ca 0.116,Mg 0.568,Fe 0.316). This cation distribution gives an equilibrium temperature of 800℃ by plotting the K value of PCA82506 on the distribution isotherm of SAXENA et al. (Earth Planet. Sci. Lett., 21,194,1974). The PCA82506 pigeonites may have cooled more rapidly than terrestrial pigeonites from the Isle of Mull and almost as rapid as the most rapidly cooled mare basalts. Report Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Mull ENVELOPE(-63.058,-63.058,-74.536,-74.536) Pecora Escarpment ENVELOPE(-68.707,-68.707,-85.639,-85.639) |
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Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
PCA82506 is relatively unshocked compared with most ureilites. Large unshocked pigeonite and olivine crystals were studied by means of single crystal X-ray diffraction, analytical TEM, optical microscope and an electronprobe. The chemical compositions of the PCA82506 pigeonites are (Ca)_6(Mg)_<76>(Fe)_<18>, while the average olivine core composition is (Fa)_<20>. A region about 50 micrometer apart from the olivine rim is reduced by the carbonaceous (C) matrix. From the diffusion profiles of olivine crystals, a cooling rate of 10-15℃/h is estimated by the computer simulation method of MIYAMOTO et al. (Proc. Lunar Planet. Sci. Conf., 16th, Pt. 1,D116,1985). The cell dimensions of the PCA82506 pigeonite determined from 23 reflections are : a, 9.6649(9); b, 8.8719(6); c, 5.2134(5)A; and β, 108.51(6)°. The site occupancy factors are M1 (Mg 0.064,Fe 0.936) and M2 (Ca 0.116,Mg 0.568,Fe 0.316). This cation distribution gives an equilibrium temperature of 800℃ by plotting the K value of PCA82506 on the distribution isotherm of SAXENA et al. (Earth Planet. Sci. Lett., 21,194,1974). The PCA82506 pigeonites may have cooled more rapidly than terrestrial pigeonites from the Isle of Mull and almost as rapid as the most rapidly cooled mare basalts. |
format |
Report |
author |
Toyoda,Hiromi Haga,Nobuhiko Tachikawa,Osamu Takeda,Hiroshi Ishii,Teruaki |
spellingShingle |
Toyoda,Hiromi Haga,Nobuhiko Tachikawa,Osamu Takeda,Hiroshi Ishii,Teruaki Thermal history of ureilite, Pecora Escarpment 82506 deduced from cation distribution and diffusion profile of minerals |
author_facet |
Toyoda,Hiromi Haga,Nobuhiko Tachikawa,Osamu Takeda,Hiroshi Ishii,Teruaki |
author_sort |
Toyoda,Hiromi |
title |
Thermal history of ureilite, Pecora Escarpment 82506 deduced from cation distribution and diffusion profile of minerals |
title_short |
Thermal history of ureilite, Pecora Escarpment 82506 deduced from cation distribution and diffusion profile of minerals |
title_full |
Thermal history of ureilite, Pecora Escarpment 82506 deduced from cation distribution and diffusion profile of minerals |
title_fullStr |
Thermal history of ureilite, Pecora Escarpment 82506 deduced from cation distribution and diffusion profile of minerals |
title_full_unstemmed |
Thermal history of ureilite, Pecora Escarpment 82506 deduced from cation distribution and diffusion profile of minerals |
title_sort |
thermal history of ureilite, pecora escarpment 82506 deduced from cation distribution and diffusion profile of minerals |
publisher |
Mineralogical Institute, Faculty of Sciences, University of Tokyo/Mineralogical Institute, Faculty of Sciences, University of Tokyo/Mineralogical Institute, Faculty of Sciences, University of Tokyo/Mineralogical Institute, Faculty of Sciences, University of Tokyo/Ocean Research Institute, University of Tokyo |
publishDate |
1986 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1965 http://id.nii.ac.jp/1291/00001965/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1965&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(-63.058,-63.058,-74.536,-74.536) ENVELOPE(-68.707,-68.707,-85.639,-85.639) |
geographic |
Mull Pecora Escarpment |
geographic_facet |
Mull Pecora Escarpment |
genre |
Memoirs of National Institute of Polar Research Polar Research |
genre_facet |
Memoirs of National Institute of Polar Research Polar Research |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1965 http://id.nii.ac.jp/1291/00001965/ AA00733561 Memoirs of National Institute of Polar Research. Special issue, 41, 206-221(1986-07) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1965&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766067785728786432 |