An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body
P(論文) An inclusion in ALH-77004 (H4 chondrite) consists of four different constituents with varying degree of recrystallization; (1) moderately to highly recrystallized lithic and chondrule fragments (fayalite-rich group), (2) unequilibrated chondrules (fayalite-poor group), (3) fine-grained dark cl...
| Main Author: | |
|---|---|
| Language: | English |
| Published: |
1983
|
| Subjects: | |
| Online Access: | https://nipr.repo.nii.ac.jp/record/1550/files/KJ00000012183.pdf |
| id |
ftnipr:oai:nipr.repo.nii.ac.jp:00001550 |
|---|---|
| record_format |
openpolar |
| spelling |
ftnipr:oai:nipr.repo.nii.ac.jp:00001550 2024-09-09T19:51:59+00:00 An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body Matsunami, Satoshi 1983-12 application/pdf https://nipr.repo.nii.ac.jp/record/1550/files/KJ00000012183.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 30 36 44 AA00733561 https://nipr.repo.nii.ac.jp/record/1550/files/KJ00000012183.pdf 1983 ftnipr 2024-06-17T04:00:49Z P(論文) An inclusion in ALH-77004 (H4 chondrite) consists of four different constituents with varying degree of recrystallization; (1) moderately to highly recrystallized lithic and chondrule fragments (fayalite-rich group), (2) unequilibrated chondrules (fayalite-poor group), (3) fine-grained dark clastic matrix, and (4) particles of Fe-Ni metal, troilite, and chromite. From petrological examinations of these constituents, it is suggested that the inclusion was a surface regolith of the L chondrite parent body formed by repetitive impact cratering processes extended to various depths of the body. 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) An inclusion in ALH-77004 (H4 chondrite) consists of four different constituents with varying degree of recrystallization; (1) moderately to highly recrystallized lithic and chondrule fragments (fayalite-rich group), (2) unequilibrated chondrules (fayalite-poor group), (3) fine-grained dark clastic matrix, and (4) particles of Fe-Ni metal, troilite, and chromite. From petrological examinations of these constituents, it is suggested that the inclusion was a surface regolith of the L chondrite parent body formed by repetitive impact cratering processes extended to various depths of the body. departmental bulletin paper |
| author |
Matsunami, Satoshi |
| spellingShingle |
Matsunami, Satoshi An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body |
| author_facet |
Matsunami, Satoshi |
| author_sort |
Matsunami, Satoshi |
| title |
An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body |
| title_short |
An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body |
| title_full |
An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body |
| title_fullStr |
An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body |
| title_full_unstemmed |
An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body |
| title_sort |
inclusion of alh-77004: a possible surface regolith of l chondrite parent body |
| publishDate |
1983 |
| url |
https://nipr.repo.nii.ac.jp/record/1550/files/KJ00000012183.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 30 36 44 AA00733561 https://nipr.repo.nii.ac.jp/record/1550/files/KJ00000012183.pdf |
| _version_ |
1809921335400333312 |