{"id":7077,"date":"2020-04-03T08:23:44","date_gmt":"2020-04-02T23:23:44","guid":{"rendered":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/?page_id=7077"},"modified":"2020-11-25T10:02:55","modified_gmt":"2020-11-25T01:02:55","slug":"master-2017","status":"publish","type":"page","link":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/education\/master\/master-2017\/","title":{"rendered":"2017\u5e74\u5ea6 \u4fee\u58eb\u8ad6\u6587"},"content":{"rendered":"

\u963f\u90e8 \u5468\u5e73<\/h3>\n

In-situ stress in the close vicinity of source fault in South African deep gold mine
\n\uff08\u5357\u30a2\u30d5\u30ea\u30ab\u5927\u6df1\u5ea6\u91d1\u9271\u5c71\u306b\u304a\u3051\u308b\u9707\u6e90\u65ad\u5c64\u76f4\u8fd1\u306e\u305d\u306e\u5834\u5fdc\u529b\uff09<\/p>\n

\u5c71\u4e0b \u6167<\/h3>\n

2016\u5e74\u718a\u672c\u5730\u9707\u9707\u6e90\u57df\u3068\u30de\u30f3\u30c8\u30eb\u6700\u4e0b\u90e8\u306e\u7570\u65b9\u6027\u30c8\u30e2\u30b0\u30e9\u30d5\u30a3\u30fc
\n\uff08Anisotropic tomography of the 2016 Kumamoto earthquake area and the lowermost mantle\uff09<\/p>\n

\u4f50\u85e4 \u5c06<\/h3>\n

\u30cb\u30e5\u30fc\u30b8\u30fc\u30e9\u30f3\u30c9\u5357\u5cf6\u5317\u90e8\u306e2016\u5e74\u30ab\u30a4\u30b3\u30a6\u30e9\u5730\u9707\u9707\u6e90\u57df\u304a\u3088\u3073\u305d\u306e\u5468\u8fba\u306b\u304a\u3051\u308b\u5fdc\u529b\u5834\u306e\u63a8\u5b9a
\n\uff08Stress tensor inversion in and around the focal area of the 2016 Kaikoura earthquake in the northern part of South Island, New Zealand\uff09<\/p>\n

\u9ad8\u6a4b \u79c0\u66a2<\/h3>\n

\u77ed\u5468\u671f\u6d77\u5e95\u5730\u9707\u8a08\u3092\u7528\u3044\u305f\u65e5\u672c\u6d77\u6e9d\u306b\u304a\u3051\u308b\u8d85\u4f4e\u5468\u6ce2\u5730\u9707\u6d3b\u52d5\u306e\u7814\u7a76
\n\uff08The activity of very low frequency earthquakes along Japan trench revealed by short-period ocean bottom seismograms\uff09<\/p>\n

\u5927\u53cb \u5468\u5e73<\/h3>\n

\u5317\u897f\u592a\u5e73\u6d0b\u306b\u304a\u3051\u308b\u6d77\u6d0b\u6027\u5730\u6bbb\u306e\u4e0d\u5747\u8cea\u6027\u306b\u95a2\u3059\u308b\u7814\u7a76
\n\uff08A study on heterogeneity of the oceanic crust in the northwestern Pacific \uff09<\/p>\n","protected":false},"excerpt":{"rendered":"

\u963f\u90e8 \u5468\u5e73 In-situ stress in the close vicini … \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\/7077"}],"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=7077"}],"version-history":[{"count":4,"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/pages\/7077\/revisions"}],"predecessor-version":[{"id":7757,"href":"http:\/\/cms1.aob.geophys.tohoku.ac.jp\/wp-json\/wp\/v2\/pages\/7077\/revisions\/7757"}],"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=7077"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}