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Hokkaido University Collection of Scholarly and Academic Papers >
Graduate School of Science / Faculty of Science >
Peer-reviewed Journal Articles, etc >
火星の真の極移動に伴う地殻変動について
| Title: | 火星の真の極移動に伴う地殻変動について |
| Other Titles: | Crustal deformation of Mars associated with the true polar wander |
| Authors: | 菅原, 守1 Browse this author | | 日置, 幸介2 Browse this author →KAKEN DB |
| Authors(alt): | Sugawara, Mamoru1 | | Heki, Kosuke2 |
| Issue Date: | 2008 |
| Publisher: | 日本測地学会 |
| Journal Title: | 測地学会誌 |
| Volume: | 54 |
| Start Page: | 279 |
| End Page: | 282 |
| Abstract: | Large scale true polar wander episodes are considered to have occurred several times in Mars. Because they accompany relocation of the Martian equatorial bulge, milli-strain level horizontal extension/compression is expected to have occurred as well as kilometer scale vertical crustal movements. Here we pick up one of such episodes reported by Perron et al. (2007), and try to compare the expected strikes of faults with those observed in satellite images. Wrinkle ridges seem to have preferred orientations aligned with the meridian connecting the present and ancient poles, which suggests that some of those may reflect the crustal stress imposed by this true polar wander episode. |
| Type: | article (author version) |
| URI: | http://hdl.handle.net/2115/35569 |
| Appears in Collections: | 理学院・理学研究院 (Graduate School of Science / Faculty of Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)
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Submitter: 日置 幸介
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