WEKO3
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Re-analysis of deep moonquakes using the Lunar Surface Gravimeter
https://jaxa.repo.nii.ac.jp/records/20405
https://jaxa.repo.nii.ac.jp/records/204056c60728f-6e08-4146-9779-cea748dd3336
Item type | 会議発表論文 / Conference Paper(1) | |||||
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公開日 | 2015-03-26 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Re-analysis of deep moonquakes using the Lunar Surface Gravimeter | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_5794 | |||||
資源タイプ | conference paper | |||||
アクセス権 | ||||||
アクセス権 | metadata only access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
著者 |
川村, 太一
× 川村, 太一× 田中, 智× 斎藤, 靖之× 小林, 佑輔× Kawamura, Taichi× Tanaka, Satoshi× Saito, Yasuyuki× Kobayashi, Yusuke× Hagermann, Axel |
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著者所属 | ||||||
東京大学 | ||||||
著者所属 | ||||||
宇宙航空研究開発機構宇宙科学研究本部 | ||||||
著者所属 | ||||||
宇宙航空研究開発機構宇宙科学研究本部 | ||||||
著者所属 | ||||||
東京大学 | ||||||
著者所属(英) | ||||||
en | ||||||
University of Tokyo | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA)(ISAS) | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA)(ISAS) | ||||||
著者所属(英) | ||||||
en | ||||||
University of Tokyo | ||||||
著者所属(英) | ||||||
en | ||||||
Open University | ||||||
出版者 | ||||||
出版者 | 宇宙航空研究開発機構宇宙科学研究本部 | |||||
出版者(英) | ||||||
出版者 | Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA) | |||||
書誌情報 |
en : Proceedings of the ISAS lunar and planetary symposium 巻 41, p. 105-113, 発行日 2009 |
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会議概要(会議名, 開催地, 会期, 主催者等)(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The 41st ISAS Lunar and Planetary Symposium (August 6-8, 2008. Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA)) | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The internal structure of the Moon is an essential piece of information that infer the origin and evolution of the Moon. Many attempts have been made for its estimation and seismic analysis using the data from Apollo Passive Seismic Experiment (PSE) is one of the most successful methods carried out. We have been focusing on the possibility of seismic use of the Lunar Surface Gravimeter (LSG) data of Apollo 17. In this study we dealt with seismic analysis of deep moonquakes and searched for possibility of the seismic use of the LSG data for deep moonquakes. We examined events from source regions A01, A06, A07, and A22. We found that 38 events out of 99 events were detected by the LSG. With 31 events, we also constructed travel time curves and tested the estimation and classification of previous study. Our result supported the previous result. We also examined some unclassified events and found events that were detected by the LSG. The detection of the signals implies the possibility of classification of unclassified events using the LSG. | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA12268968 | |||||
資料番号 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 資料番号: AA0064291026 |