Bibliografie tematiche / Kinkai kikan

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Letteratura scientifica selezionata sul tema "Kinkai kikan"

Autore: Grafiati
Pubblicato: 29 luglio 2024
Ultima modifica: 30 luglio 2024

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Articoli di riviste sul tema "Kinkai kikan"

1

GOTO, Kazuhiko, Chikara SHIMIZU, Tsuyoshi NAKATSUJI, Toshihiko KANAZAWA, Tomoaki YAMADA, Hideki SHIMAMURA, Hajime SHIOBARA et al. "the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. Activity of the 1995 Amami-Oshima-Kinkai Earthquakes." Journal of Geography (Chigaku Zasshi) 106, n. 4 (1997): 503–13. http://dx.doi.org/10.5026/jgeography.106.4_503.

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2

TAKENAKA, Hiroshi, Yushiro FUJII, Takashi OKUMURA e Sadaomi SUZUKI. "the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. Modelling of Strong Motion at Kikai Island due to Aftershocks of the 1995 Amami-Oshima-Kinkai Earthquakes." Journal of Geography (Chigaku Zasshi) 106, n. 4 (1997): 525–36. http://dx.doi.org/10.5026/jgeography.106.4_525.

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3

KAKUTA, Toshiki, Kazuhiko GOTO, Hiroki MIYAMACHI, Syuichiro HIRANO, Chikara SHIMIZU, Kazuhiro IWAKIRI, Tsuyoshi NAKATSUJI e Seiji TATEYAMA. "the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. The 1995 Amami-Oshima-Kinkai Earthquake-Activities and damage." Journal of Geography (Chigaku Zasshi) 106, n. 4 (1997): 476–85. http://dx.doi.org/10.5026/jgeography.106.4_476.

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4

SATAKE, Kenji, e Yuichiro TANIOKA. "the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. Fault Parameters and Tsunami Generation of the 1995 Amami-Oshima-Kinkai Earthquake." Journal of Geography (Chigaku Zasshi) 106, n. 4 (1997): 546–56. http://dx.doi.org/10.5026/jgeography.106.4_546.

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5

YAMADA, Tomoaki, Ryota HINO, Azusa NISHIZAWA, Hajime SHIOBARA, Toshinori SATO, Kazuhiko GOTO, Toshihiko KANAZAWA, Junzo KASAHARA e Hideki SHIMAMURA. "the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. Aftershock Observation of the 1995 Amami-Oshima-Kinkai Earthquake Using Ocean Bottom Seismometers." Journal of Geography (Chigaku Zasshi) 106, n. 4 (1997): 514–24. http://dx.doi.org/10.5026/jgeography.106.4_514.

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KIKUCHI, Masayuki. "the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. Rupture Process of the 1995 Amami-Oshima-Kinkai Earthquakes Inferred from Teleseismic Data." Journal of Geography (Chigaku Zasshi) 106, n. 4 (1997): 537–45. http://dx.doi.org/10.5026/jgeography.106.4_537.

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7

KASAHARA, Junzo, e Toshinori SATO. "the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. A Subducting Seamount and Its Tectonic Influence to the 1995 Amami-Oshima-Kinkai Earthquake." Journal of Geography (Chigaku Zasshi) 106, n. 4 (1997): 557–66. http://dx.doi.org/10.5026/jgeography.106.4_557.

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8

HARADA, K. "Kindai Nihon to Kika Seido (Naturalization in Modern Japan)". Social Science Japan Journal 11, n. 2 (3 novembre 2008): 319–22. http://dx.doi.org/10.1093/ssjj/jyn055.

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TSUJI, Yoshinobu. "the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. Damage to Villages on Amami Archipelago due to the 1995 Amami-Oshima-Kinkai Earthquake-Tsunami." Journal of Geography (Chigaku Zasshi) 106, n. 4 (1997): 486–502. http://dx.doi.org/10.5026/jgeography.106.4_486.

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MENEZES FILHO, Antonio Carlos Pereira de, e Carlos Frederico de Souza CASTRO. "CARACTERIZAÇÃO QUÍMICA E ATIVIDADE ANTIFÚNGICA DOS ÓLEOS ESSENCIAIS DE LARANJA-KINKAN (Fortunella margarita (LOUR.) SWINGLE)". Folia Amazónica 28, n. 2 (15 settembre 2020): 185–98. http://dx.doi.org/10.24841/fa.v28i2.482.

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Abstract (sommario):
A laranja-kinkan (Fortunella margarita) é bem conhecida pelo fruto comestível e rico em antioxidantes, mas muitos outros usos benéficos ainda precisam ser investigados. Neste estudo, empregamos cromatografia gasosa com espectrometria de massas (CG-MS), para avaliar o potencial antifúngico dos óleos essenciais dos frutos verde e maduro para inibir efetivamente os patógenos vegetais: Colletotrichum acutatum, C. gloeosporioides e Sclerotinia sclerotiorum. Frutos verdes e maduros de F. margarita foram coletados em uma unidade rural no município de Rio Verde, Goiás, Brasil. Adicionalmente, o rendimento de óleo essencial foi determinado por hidrodestilação em sistema tipo Clevenger. Foram obtidos rendimentos de óleos essenciais de 3,57 e 3,64% para os frutos verde e maduro. No perfil químico foram observados seis compostos majoritários β-pineno, limoneno, β-felandreno, α-guaieno, germacreno D e biciclosesquifelandreno para ambas as amostras. Os óleos essenciais apresentaram alta eficiência no percentual de inibição contra os três patógenos fúngicos. Portanto, os óleos essenciais dos frutos verde e maduro da laranja-Kinkan podem ter aplicações antifúngicas.
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Più fonti

Libri sul tema "Kinkai kikan"

1

1925-, Fujisawa Norio, e Bukkyō Bijutsu Kenkyū Ueno Kinen Zaidan. Josei Kenkyūkai., a cura di. Shaka kinkan shutsugenzu: Kenkyū happyō to zadankai. Kyōto-shi: Bukkyō Bijutsu Kenkyū Ueno Kinen Zaidan Josei Kenkyūkai, 1993.

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2

1925-, Fujisawa Norio, e Bukkyō Bijutsu Kenkyū Ueno Kinen Zaidan. Josei Kenkyūkai., a cura di. Shaka kinkan shutsugenzu: Kenkyū happyō to zadankai. Kyōto-shi: Bukkyō Bijutsu Kenkyū Ueno Kinen Zaidan Josei Kenkyūkai, 1993.

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3

Bukkyō Bijutsu Kenkyū Ueno Kinen Zaidan. Josei Kenkyūkai, a cura di. Shaka kinkan shutsugenzu: Kenkyū happyō to zadankai. Kyōto-shi: Bukkyō Bijutsu Kenkyū Ueno Kinen Zaidan Josei Kenkyūkai, 1993.

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4

Hida Yoshifumi...[et al.]. Kindai no goi ; 2: Nihongo no kihan gadekiru jidai. Tokyo: Asakura Shoten, 2022.

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5

Nagai, Yumi. Kindai Nihon hoikusha yōseishi no kenkyū: Kirisutokyō-kei hobo yōsei kikan o chūshin ni. Tōkyō: Kazama Shobō, 2016.

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6

Oyama, Naoko. Furokku kōto to haorihakama: Reisō kihan no keisei to kindai Nihon. Tōkyō: Keisō Shobō, 2016.

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7

Japan. Kinki Keizai Sangyōkyoku. Sangakukan Renkei Suishinka., a cura di. Kinki chiiki ni okeru chūshō kigyō no kōsetsu shiken kenkyū kikan no riyō jittai to gijutsu shien no jūjitsuka hōsaku ni tsuite: Kinki chiiki ni okeru kōsetsu shiken kenkyū kikan to ta kikan to no renkei ni yoru gijutsu shīzu no jigyōka kanōsei chōsa : hōkokusho. Ōsaka-shi: Kinki Keizai Sangyōkyoku, 2006.

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8

Tomura, Osamu. Senzenki Waseda, Keiō no keiei: Kindai Nihon shiritsu kōtō kyōiku kikan ni okeru kyōiku to zaimu no sōkoku. Kyōto-shi: Mineruva Shobō, 2017.

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9

author, Ueda Aya 1964, Aoki Mihoko author e Kyōto Kōgei Sen'i Daigaku. Bijutsu Kōgei Shiryōkan, a cura di. Kindai zuanchō: Terada Tetsuo korekushon ni miru, kikai nassen no sekai = Book of contemporary designs. Kyōto-shi: Seigensha, 2020.

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10

Sangyōkyoku, Japan Kinki Keizai. Kinki chiiki ni okeru minkan shien bijinesu no ikusei to kōteki kikan to no nettowāku kōchiku ni yoru benchā shiensaku no kōkateki na tenkai ni kansuru chōsa kenkyū: Hōkokusho : Heisei 12-nendo chiiki shinki jigyō hatten kiban chōsa. [Osaka?]: Kinki Keizai Sangyōkyoku, 2001.

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Capitoli di libri sul tema "Kinkai kikan"

1

Mashima, Hidehisa. "Forearc magmatism along southwest Japan is caused by rupturing of the subducting slab". In In the Footsteps of Warren B. Hamilton: New Ideas in Earth Science. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2553(33).

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Abstract (sommario):
ABSTRACT The genesis of the forearc magmatism in southwest Japan at 14 Ma was studied using geologic and seismic observations. Before the magmatism, the Shimanto accretionary complexes were uplifted by 1000–3000 m between 21 and 17 Ma during the opening of the Japan Sea and the Shikoku Basin. Opening of the Japan Sea and the Shikoku Basin terminated at 15 Ma, when the Kinan Seamount Chain on the Shikoku Basin activated. The magmatic products are distributed at segment boundaries and in aseismic areas of the subducting Philippine Sea plate. The segment boundaries are located on syncline and anticline axes of the subducting slab at Kyushu. The magmatic products at Shikoku are distributed at places where olistostromes uplifted between 21 and 17 Ma. Beneath the Kumano volcanic rocks at Kii, a significant discontinuity in the locations of deep earthquakes is observed. These observations indicate that rupturing of the subducting slab by the load of the overriding plate occurred at around 14 Ma. The slab rupturing would have enabled subslab asthenosphere and/or magma to be injected into the plate interface through the tear and cause the forearc magmatism. Since the oceanic plate has a number of preexisting weaknesses, such as fracture zones, slab rupturing could occur more commonly than previously considered. The forearc magmatism caused by slab rupture is an important process associated with the growth of continental crust in subduction zones.
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Atti di convegni sul tema "Kinkai kikan"

1

Kawaldi, Rendy Shika, Mohamad Miftahuddin Muazaki e Akmal Rahmanto. "Tinjauan Permasalahan Pengelolaan pada Bangunan Rusunawa di Indonesia". In Temu Ilmiah IPLBI 2021. Ikatan Peneliti Lingkungan Binaan Indonesia, 2021. http://dx.doi.org/10.32315/ti.9.c019.

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Abstract (sommario):
Setiap manusia memiliki insting untuk bertahan hidup. Oleh karena itu, mereka membangun sebuah shelter atau tempat untuk berlindung sebagai kebebasan mereka untuk beraktivitas di dalamnya yang dibatasi oleh privasi. Hal itu didukungnya dengan evolusi sebuah tempat tinggal yang awalnya sangat sederhana hingga termodernisasi oleh berkembangnya pemikiran serta akal manusia. Pembangunan sudah beragam di era yang modern ini. Salah satunya proyek pembangunan hunian vertikal yang sudah terealisasikan di beberapa tempat. Tuntutan pola hidup tradisional dengan pendapatan rakyat yang dibawah rata-rata diwadahi pemerintah dengan cara membangun rumah susun. Rumah bertingkat dengan satu lingkungan tempat hunian kini juga merupakan salah satu solusi untuk mengatasi ketersediaan lahan yang kian menipis. Kata-kunci : peninjauan, pengelola, rusunawa, hunian, vertikal
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