Human Behavior after the 2018 Osaka Earthquake

This study examined human behavior after the 2018 Osaka earthquake. The 2018 Osaka Earthquake was the first earthquake that struck an urban area during morning commuting hours in Japan. The internet questionnaire survey was carried out for the 500 people who used the railway in the earthquake occurrence. It was found that 60.4 percent of people went to work and 39.6 percent of people returned home. There were many people who answered that they went home because it was impossible to go to the office. It can be said that most Japanese think that they should go to work even if an earthquake occurs. Because the Internet was available during the earthquake, many people collected information with their smartphones. It was indicated that the anxiety and confusion were little even in the situation where people were confined in the train and the train did not move.本研究は、2018年度関西大学教育研究緊急支援経費による助成を受けた

Culicidae y Ceratopogonidae (Diptera: Nematocera) que habitan en fi totelmata en el Parque Nacional Iguazú, provincia de Misiones, Argentina subtropical

A list of the most common phytotelmata and their Culicidae and Ceratopogonidae inhabitants from Iguazú National Park, Misiones Province, Argentina, is presented, and biological and behavioral observations are also included. Species of Poaceae, Bromeliaceae, Apiaceae, Araceae, Urticaceae, Marantaceae, and Arecaceae, were identified as phytotelmata. Twenty six species of Culicidae and nine of Ceratopogonidae were identified. The highest species richness of culicids and ceratopogonids was recorded from the bamboo Guadua chacoensis (Poaceae) and treeholes, respectively. Fourteen species of Culicidae and three of Ceratopogonidae inhabit bamboo, two and five treeholes, seven and three bromeliads, and nine and one, other less known phytotelmata, respectively.Se presenta una lista de las fitotelmata más comunes y los Culicidae y Ceratopogonidae que las habitan, del Parque Nacional Iguazú, Misiones, Argentina; además de observaciones biológicas y de comportamiento. Especies de Poaceae, Bromeliaceae, Apiaceae, Araceae, Urticaceae, Marantaceae, y Arecaceae, fueron identificadas como fitotelmata. Fueron reconocidas 26 especies de culícidos y nueve de Ceratopogonidae. La mayor riqueza de especies de culícidos y ceratopogónidos se registraron en el bambú Guadua chacoensis (Poaceae) y en los huecos de los árboles respectivamente. Catorce especies de culícidos y tres de ceratopogónidos habitan bambúes, dos y cinco en los huecos de los árboles, siete y tres en bromelias y nueve y una en otras fitotelmata, respectivamente.Fil: Campos, Raul Ernesto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Instituto de Limnología "Dr. Raúl A. Ringuelet". Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Limnología; ArgentinaFil: Spinelli, Gustavo Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Instituto de Limnología "Dr. Raúl A. Ringuelet". Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Limnología; ArgentinaFil: Mogi, Motoyoshi. Saga University; Japó

Electron microprobe technique for U-Th-Pb and REE chemistry of monazite, and its implications for pre-, peak- and post- metamorphic events of the Lutzow-Holm Complex and the Napier Complex, East Antarctica

Monazites in high-grade metapelites from the Lutzow-Holm Complex and Napier Complex have been examined in terms of U, Th, Pb and rare earth element (REE) chemistry using an electron microprobe. The studied samples include four granulite-facies garnet-biotite-bearing metapelites from Skallen within the Lutzow-Holm Complex, and a re-hydrated garnet-sillimanite gneiss from the Mt. Riiser-Larsen area within the UHT zone of the Napier Complex. Two out of four garnet-bearing metapelitic samples from Skallen gave simple 560-500Ma monazite U-Th-Pb ages, whereas the other two samples yielded two age populations, i.e., 560-500Ma and 650-580Ma. The younger age group is consistent with the 550-520Ma metamorphic ages reported by SHRIMP. The older>580Ma monazites are relatively enriched in Nd, Sm, Gd, Dy (MREE) and depleted in Si (Ca and Th) compared with the younger (560-500Ma) ones. These older monazites possibly formed through M-HREE-enriched conditions such as garnet-free conditions, suggesting that the growth of these monazites pre-dated the peak metamorphism. Garnet-sillimanite gneiss from the Mt. Riiser-Larsen area shows various post-UHT re-hydration textures such as biotite-sillimanite aggregates, and fine-grained biotite flakes around or intracrystalline fractures within garnet porphyroblasts. Monazites enclosed within garnet cores have 2480-2440Ma U-Th-Pb ages consistent with the reported zircon and monazite SHRIMP dates. On the other hand, those associated with re-hydrated zones gave fluctuating 2200-700Ma ages. These younger ages are thought to reflect the incomplete chemical disturbance during the post-UHT crustal processes

TiO2 solubility in garnet coexisting with orthopyroxene, quartz and rutile: Ti-in-garnet thermometer for ultrahigh-temperature granulites

第6回極域科学シンポジウム[OG] 地圏11月16日（月）　国立極地研究所１階交流アトリウ