{"id":8461,"date":"2022-03-25T09:38:54","date_gmt":"2022-03-25T00:38:54","guid":{"rendered":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/?page_id=8461"},"modified":"2022-04-04T10:13:26","modified_gmt":"2022-04-04T01:13:26","slug":"master-2020","status":"publish","type":"page","link":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/education\/master\/master-2020\/","title":{"rendered":"2020\u5e74\u5ea6 \u4fee\u58eb\u8ad6\u6587"},"content":{"rendered":"

\u5927\u585a \u82f1\u4eba<\/h3>\n

\u6d77\u5e95\u6c34\u5727\u8a08\u30c7\u30fc\u30bf\u306b\u8a18\u9332\u3055\u308c\u308b\u975e\u6f6e\u6c50\u6d77\u6d0b\u6210\u5206\u306e\u6642\u7a7a\u9593\u7279\u5fb4\u306b\u95a2\u3059\u308b\u7814\u7a76
\n\uff08A study on spatio-temporal characteristics of the non-tidal oceanographical
\nfluctuation recorded in ocean bottom pressure sensors\uff09<\/p>\n

\u7247\u5c71 \u60a0<\/h3>\n

S-net\u3068Hi-net\u30c7\u30fc\u30bf\u3092\u7528\u3044\u305f\u6771\u65e5\u672c\u524d\u5f27\u57df\u306e\u901f\u5ea6\u69cb\u9020\u306e\u7814\u7a76
\n\uff08Seismic structure of the East Japan forearc derived from S-net and Hi-net data\uff09<\/p>\n

\u6728\u6751 \u53cb\u5b63\u4fdd<\/h3>\n

GNSS-\u97f3\u97ff\u6e2c\u8ddd\u306e\u65b0\u3057\u3044\u6d77\u5e95\u5c40\u914d\u7f6e\u306e\u63d0\u6848\u3068\u5343\u5cf6\u6d77\u6e9d\u6839\u5ba4\u6c96\u3067\u306e\u89b3\u6e2c\u3078\u306e\u9069\u7528
\n\uff08A new transponder layout in GNSS-acoustic survey and its application to observations at off Nemuro, Kuril trench\uff09<\/p>\n

\u7530\u4e0a \u7dbe\u9999<\/h3>\n

\u65e5\u672c\u6d77\u6771\u7e01\u5730\u57df\u306e\u5fdc\u529b\u5834\u3068\u767a\u751f\u3057\u305f\u5730\u9707\u306e\u65ad\u5c64\u9762\u3068\u306e\u95a2\u4fc2
\n\uff08Stress field in the eastern margin of the Japan Sea and its relationship with faults of recent earthquakes\uff09<\/p>\n

\u677e\u91ce \u5f25\u611b<\/h3>\n

2016\u5e74\u30cb\u30e5\u30fc\u30b8\u30fc\u30e9\u30f3\u30c9\u30fb\u30ab\u30a4\u30b3\u30a6\u30e9\u5730\u9707\u9707\u6e90\u57df\u306b\u304a\u3051\u308b\u5fdc\u529b\u5834\u306e\u6642\u7a7a\u9593\u5909\u5316
\n\uff08Spatial and temporal change of stress field in the focal area of the 2016 Kaikoura earthquake, New Zealand\uff09<\/p>\n","protected":false},"excerpt":{"rendered":"

\u5927\u585a \u82f1\u4eba \u6d77\u5e95\u6c34\u5727\u8a08\u30c7\u30fc\u30bf\u306b\u8a18\u9332\u3055\u308c\u308b\u975e\u6f6e\u6c50\u6d77\u6d0b\u6210\u5206\u306e\u6642\u7a7a\u9593\u7279\u5fb4\u306b\u95a2\u3059\u308b\u7814\u7a76 … \u7d9a\u304d\u3092\u8aad\u3080 →<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":113,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/pages\/8461"}],"collection":[{"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/comments?post=8461"}],"version-history":[{"count":3,"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/pages\/8461\/revisions"}],"predecessor-version":[{"id":8489,"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/pages\/8461\/revisions\/8489"}],"up":[{"embeddable":true,"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/pages\/113"}],"wp:attachment":[{"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/media?parent=8461"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}