{"id":353,"date":"2002-01-01T11:40:08","date_gmt":"2002-01-01T02:40:08","guid":{"rendered":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/?p=353"},"modified":"2018-08-21T15:48:08","modified_gmt":"2018-08-21T06:48:08","slug":"2002publication","status":"publish","type":"post","link":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/2002publication\/","title":{"rendered":"2002"},"content":{"rendered":"<p>1.Parallelepiped cooling joint and anisotropy of P-wave velocity in the Takidani granitoid, Japan Alps<br \/>\n[Journal of Volcanology and Geothermal Research, 114, (2002), 465-477]\nShingo Kano and Noriyoshi Tsuchiya<\/p>\n<p>2.Rb-Sr and Sm-Nd Mineral Isochron Ages of the Metamorphic Rocks in the Namaqualand Metamorphic Complex, South Africa<br \/>\n[Gondwana Research, 5 (4), (2002), 771-779]\nM. Yuhara, T. Miyazaki, J. Ishioka, S. Suzuki, H. Kagami and N. Tsuchiya<\/p>\n<p>3.Experimental Approach to Hydrothermally Derived Fracturing of Granitic Rock for Enhanced Geothermal Reservoir Systems<br \/>\n[Geothermal Resources Council Transactions, 26, (2002), 285 &#8211; 288]\nN. Hirano, A. Minakawa, G. Bignall, N. Yamasaki, N. Tsuchiya and K. Nakatsuka<\/p>\n<p>4.Anisotropy of Cooling Joint Systems in Granite<br \/>\n[Geothermal Resources Council Transactions, 26, (2002), 309 &#8211; 314]\nS. Kano, G. Bignall and N. Tsuchiya<\/p>\n<p>5.HYDROTHERMAL QUARTZ MICROTEXTURES AND DEPOSITIONAL PROCESSES REVEALED BY SEM-CL IMAGING<br \/>\n[Proceedings 24th New Zealand Geothermal Workshop, 24, (2002), 223-228]\nG. BIGNALL, K. SEKINE, N. TSUCHIYA<\/p>\n<p>6.APPLICATION OF THERMOLUMINESCENCE TECHNIQUE TO GEOTHERMAL EXPLORATION<br \/>\n[Proceedings 24th New Zealand Geothermal Workshop, 24, (2002), 85-90]\nN. TSUCHIYA, K. NAKATSUKA<\/p>\n<p>7.Experimental Approach to Understanding Water-Rock Interaction in Enhanced Geothermal Systems<br \/>\n[Proceedings of 23rd New Zealand Geothermal Workshop, 23, (2001), 15-20]\nG. Bignall, N. Hirano, N. Yamasaki, N. Tsuchiya, and K. Nakatsuka<\/p>\n","protected":false},"excerpt":{"rendered":"<p>1.Parallelepiped cooling joint and anisotropy of P-wave velocity in the Takidani granitoid, Japan Alps [Journa &hellip; <\/p>\n<p class=\"link-more\"><a href=\"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/2002publication\/\" class=\"more-link\"><span class=\"screen-reader-text\">&#8220;2002&#8221; \u306e<\/span>\u7d9a\u304d\u3092\u8aad\u3080<\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[8],"tags":[],"class_list":["post-353","post","type-post","status-publish","format-standard","hentry","category-publication"],"_links":{"self":[{"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/posts\/353","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/comments?post=353"}],"version-history":[{"count":1,"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/posts\/353\/revisions"}],"predecessor-version":[{"id":354,"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/posts\/353\/revisions\/354"}],"wp:attachment":[{"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/media?parent=353"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/categories?post=353"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/geo.kankyo.tohoku.ac.jp\/gmel\/index.php\/wp-json\/wp\/v2\/tags?post=353"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}