{"id":1119,"date":"2013-06-20T15:01:01","date_gmt":"2013-06-20T06:01:01","guid":{"rendered":"http:\/\/www.jpgu.org\/en\/?p=1119"},"modified":"2018-06-25T15:06:29","modified_gmt":"2018-06-25T06:06:29","slug":"jpgu-meeting-2013-student-outstanding-presentation-awards-were-given","status":"publish","type":"post","link":"https:\/\/www.jpgu.org\/en\/news\/2013\/1119\/","title":{"rendered":"JpGU Meeting 2013 Student Outstanding Presentation Awards were given"},"content":{"rendered":"<p>Student Outstanding Presentation Awards were given !<\/p>\n<p>We are deeply grateful for all of your presentation of splendid research outcome. We would like to express our best wishes for your continued success on your research in the future.<\/p>\n<h2 class=\"jpgu-regist\">Human Geosciences Section<\/h2>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nRupprecht Christoph<br \/>\n<\/TD><br \/>\n<TD><br \/>\nGriffith School of Environment, Griffith University<br \/>\n<\/TD><br \/>\n<TD><br \/>\nAppreciation of informal urban greenspace by Japanese and Australian residents<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nHiroto Nagai<\/TD><br \/>\n<TD><br \/>\nNagoya University <\/TD><br \/>\n<TD><br \/>\nAn ALOS-derived glacier inventory of the Bhutan Himalaya<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nMohammad Rajib<br \/>\n<\/TD><br \/>\n<TD><br \/>\nGraduate School of Science and Engineering, Saitama University<br \/>\n<\/TD><br \/>\n<TD><br \/>\nVariations in Adsorption Coefficient of  <sup>133<\/sup>Cs and <sup>87<\/sup>Sr Caused by Oxidation of Pumice Tuff<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nYuki Nakamura<\/TD><br \/>\n<TD><br \/>\nhe University of Tokyo<\/TD><br \/>\n<TD><br \/>\n3D structural analysis of large-scale submarine landslide on a very gentle continental slope off Shimokita Peninsula<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKeitaro Yamada <\/TD><br \/>\n<TD><br \/>\nKyoto University <\/TD><br \/>\n<TD><br \/>\nSedimentary environment during 3000 years recorded in the piston core sediments of Beppu Bay, central Kyushu, Japan<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nYoshiki Sato<\/TD><br \/>\n<TD><br \/>\nKyushu University <\/TD><br \/>\n<TD><br \/>\nLate Holocene environmental changes of the inter-ridge marshes in the western Hamamatsu strand plain<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><\/p>\n<p>Akihiro Yokota<\/TD><br \/>\n<TD><br \/>\nNihon University<\/TD><br \/>\n<TD><br \/>\nEruption history of Tarumae volcano and tephras since 17th century found in Shiraoi-Tomakomai lowlands<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><\/TABLE><br \/>\n<br \/>\n<\/DIV><\/p>\n<p><DIV class=\"text\"><br \/>\n<A name=\"01\"><\/p>\n<h2 class=\"jpgu-regist\">Biogeosciences Section<\/h2>\n<p><DIV class=\"text2\"><\/p>\n<p><TABLE class=\"list\"><br \/>\n<!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nMariko Harada<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<\/TD><br \/>\n<TD><br \/>\nModeling the rise of oxygen after the Snowball earth: implications for the Paleoproterozoic manganese and iron formation<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKouhei Tokunaga<\/TD><br \/>\n<TD><br \/>\nHiroshima University<\/TD><br \/>\n<TD><br \/>\nApplication of selenium coprecipitated with barite as a new redox indicator<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKeisuke Shimizu<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<\/TD><br \/>\n<TD><br \/>\nMolecular mechanisms of shell coiling in gastropods<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><\/TABLE><br \/>\n<br \/>\n<\/DIV><\/p>\n<p><DIV class=\"text\"><br \/>\n<A name=\"01\"><\/p>\n<h2 class=\"jpgu-regist\"> Atmospheric, Ocean and Environmental Sciences Section<\/h2>\n<p><DIV class=\"text2\"><\/p>\n<p><TABLE class=\"list\"><br \/>\n<!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKota Okamoto<br \/>\n<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<br \/>\n<\/TD><br \/>\n<TD><br \/>\nInterhemispheric differences in the roles of SAO in mid- and high latitudes<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nChikara Tsuchiya<br \/>\n<\/TD><br \/>\n<TD><br \/>\nhe University of Tokyo<br \/>\n<\/TD><br \/>\n<TD><br \/>\nPropagation characteristics of gravity waves in the austral winter using the AIRS high resolution data<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nRay Takatani<br \/>\n<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<br \/>\n<\/TD><br \/>\n<TD><br \/>\nSimulation of aerosol-cloud interactions in spring over East Asia using WRF-chem model : Comparison with aircraft obs.<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nTakashi Nakano<br \/>\n<\/TD><br \/>\n<TD><br \/>\nKyoto University<br \/>\n<\/TD><br \/>\n<TD><br \/>\ncean response to typhoons moving toward north in the East China Sea<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKazunori Ebata<br \/>\n<\/TD><br \/>\n<TD><br \/>\nYamanashi University<br \/>\n<\/TD><br \/>\n<TD><br \/>\nDeveloping and improving a simple runoff model of dissolved organic carbon considering soil infiltration and river runof<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nYuki Yasuda<br \/>\n<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<br \/>\n<\/TD><br \/>\n<TD><br \/>\nA theoretical study on the mechanism for spontaneous gravity wave generation using the renormalized perturbation method<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nSatoki Tsujino<br \/>\n<\/TD><br \/>\n<TD><br \/>\nNagoya University<br \/>\n<\/TD><br \/>\n<TD><br \/>\nNumerical Experiments for Concentric Eyewalls of Typhoon Bolaven (2012)<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><\/TABLE><br \/>\n<br \/>\n<\/DIV><\/p>\n<p><DIV class=\"text\"><br \/>\n<A name=\"01\"><\/p>\n<h2 class=\"jpgu-regist\">Solid Earth Section<\/h2>\n<p><DIV class=\"text2\"><\/p>\n<p><TABLE class=\"list\"><br \/>\n<!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nSho Aoki<br \/>\n<\/TD><br \/>\n<TD><br \/>\nKyoto University<br \/>\n<\/TD><br \/>\n<TD><br \/>\nThe estimation of S wave reflector in the northern Kinki region<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nNaho Otsuji<br \/>\n<\/TD><br \/>\n<TD><br \/>\nNiigata University<br \/>\n<\/TD><br \/>\n<TD><br \/>\nSr and Nd isotope systematics of metacarbonate rocks as proxies for extinct oceans in continental collision zones<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nAkiko Takeo<br \/>\n<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<br \/>\n<\/TD><br \/>\n<TD><br \/>\nShear-wave anisotropy in the crust and uppermost mantle beneath Japan from broadband array analysis of surface waves<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nNorihiro Nakata<br \/>\n<\/TD><br \/>\n<TD><br \/>\nColorado School of Mines<br \/>\n<\/TD><br \/>\n<TD><br \/>\nTime-lapse changes in velocity and anisotropy after the 2011 Tohoku earthquake estimated by seismic interferometry<br \/>\n<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKazutaka Yasukawa<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<\/TD><br \/>\n<TD><br \/>\nGeochemical features of deep-sea sediment in the eastern Indian Ocean: the first report of the Indian REY-rich mud.<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nRyuichi Nomura<\/TD><br \/>\n<TD><br \/>\nTokyo Institute of Technology<\/TD><br \/>\n<TD><br \/>\nChemical evolution of basal magma ocean and mantle structure of the early Earth<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nTaro Nizato<\/TD><br \/>\n<TD><br \/>\nHiroshima University <\/TD><br \/>\n<TD><br \/>\nStatistical hypothesis test for the detection of very low-frequency earthquakes in southwest Japan<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nRyo Tanaka<\/TD><br \/>\n<TD><br \/>\nHokkaido University<\/TD><br \/>\n<TD><br \/>\nTransition in eruption style during the 2011 eruption of Shinmoe-dake: implications from a steady conduit flow model<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nShuto Sugai<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo <\/TD><br \/>\n<TD><br \/>\nRoles of active faults for fluid-flow in the crust, examples from Chubu district, Japan<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nShuji Terusawa<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<\/TD><br \/>\n<TD><br \/>\nExamination of noble gas concentration by percolation by using ceramic membrane<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKosuke Ishige<\/TD><br \/>\n<TD><br \/>\nHokkaido University<\/TD><br \/>\n<TD><br \/>\nGeology and petrology of Taisetsu volcanic field ; Formation history and Transition of magma<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nMamoru Ozaki<\/TD><br \/>\n<TD><br \/>\nIbaraki University<\/TD><br \/>\n<TD><br \/>\nGeology and Petrology of the Post-caldera Stage Lava flows originated from Azuma-Kofuji cone, East Azuma volcano<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nMasakazu Fujii<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<\/TD><br \/>\n<TD><br \/>\nMagnetic Structure of Back-arc Spreading Axis with Hydrothermal Vents; the Southern Mariana Trough<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nTakashi Kuratomi<\/TD><br \/>\n<TD><br \/>\nKyushu University<\/TD><br \/>\n<TD><br \/>\nhe structure of chimney at iron-silica rich hydrothermal environment in shallow marine, Satsuma Iwo-Jima, Kikai caldera<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nMichiyo Sawai<\/TD><br \/>\n<TD><br \/>\nHiroshima University<\/TD><br \/>\n<TD><br \/>\nFrictional behavior of incoming pelagic sediments to the Tohoku subduction zone\t<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKazuya Ishitsuka<\/TD><br \/>\n<TD><br \/>\nKyoto University<\/TD><br \/>\n<TD><br \/>\nSurface displacements after the ground water regulation in Bangkok derived from persistent scatterer SAR interferometry<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nTakahiro Shiina<br \/>\n<\/TD><br \/>\n<TD><br \/>\nTohoku University<\/TD><br \/>\n<TD><br \/>\nP-wave velocity structure in the subducting crust of the Pacific plate beneath northeast Japan<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nNao Yasuda <\/TD><br \/>\n<TD><br \/>\nKanazawa University<\/TD><br \/>\n<TD><br \/>\nExperimental study of liquefaction and fluid transport<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><\/p>\n<p>Masahiro Kobayashi<br \/>\n<\/TD><br \/>\n<TD><br \/>\nThe University of Tokyo<\/TD><br \/>\n<TD><br \/>\nSedimentary pore fluid-like halogens and noble gases in mantle peridotites from the Western-Pacific subduction zones<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nKeisuke Yoshida<\/TD><br \/>\n<TD><br \/>\nTohoku University<\/TD><br \/>\n<TD><br \/>\nChange in the stress field in the inland area of NE Japan after the 2011 Tohoku-Oki earthquake<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nYusuke Oishi<\/TD><br \/>\n<TD><br \/>\nKochi University<\/TD><br \/>\n<TD><br \/>\nH\/V spectral analysis based on high density micro-tremor observations in Kochi Plain<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nTakafumi Nishiwaki<\/TD><br \/>\n<TD><br \/>\nHiroshima University<\/TD><br \/>\n<TD><br \/>\nMicrostructures and formation process of slickenside<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><!--\u3053\u3053\u304b\u3089--><br \/>\n<TR><br \/>\n<TD><br \/>\nNoriko Shiraishi<\/TD><br \/>\n<TD><br \/>\nEhime University<\/TD><br \/>\n<TD><br \/>\nPhase relations and density changes in mid-ocean ridge basalt (MORB) under the lower mantle condition<\/TD><br \/>\n<\/TR><br \/>\n<!--\u3053\u3053\u307e\u3067--><\/p>\n<p><\/TABLE><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Student Outstanding Presentation Awards were given ! We are deeply grateful for all of your presentation of sp [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"_links":{"self":[{"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/posts\/1119"}],"collection":[{"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/comments?post=1119"}],"version-history":[{"count":5,"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/posts\/1119\/revisions"}],"predecessor-version":[{"id":1122,"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/posts\/1119\/revisions\/1122"}],"wp:attachment":[{"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/media?parent=1119"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/categories?post=1119"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.jpgu.org\/en\/wp-json\/wp\/v2\/tags?post=1119"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}