411 research outputs found
Digitized material from "'Shin shinfujin' kaisetsu, sōmokuji, sakuin"
No full textTables of contents and author index for the eight-volume set Shin shin fujin.The Mellon Foundation - Council on East Asian Libraries Innovation Grants for East Asian Librarian
Geology of Mt. Fuji and paleomagnetism of lavas of Shin-Fuji Volcano
No full textGeologic classification and distributions of the effusives of Fuji Volcano were com-piled mainly based on Tsuya (1968,1971) and the framework of geologic age by Miyaji (1988). The effusives can be classified into those of the Ko-Fuji and Shin-Fuji Volcanos, and that of the Shin-Fuji Volcano can be divided into 3,old, middle and young. The age of the boundary between the old and middle of Shin-Fuji Volcano is ca. 6300 years, and between middle and young is ca. 2200 years. The enormous amount of effusives of Fuji Volcano is related to the collision tectonics in central Japan, induced by motion of the Philip-pine Sea Plate. Paleomagnetic samples were collected from 11 sites of the old lavas and 3 sites of the middle aged lavas of the Shin-Fuji Volcano. Three oriented blocks were sampled from each site. The intensities of natural remanent magnetization (NRM) of most of the samples ranged from 5 to 25 A/m, and median destructive field (MDF) was 15-40mT. The direction of stepwise demagnetized NRM is stable and can be used for paleomagnetic studies. The positions of the virtual geomagnetic pole (VGP) are distributed around North Pole within latitudes higher than 60°N. VGP distributions are significantly different for the sites on the "same" lava. NRM intensities, MDF, anisotropy of magnetic susceptibility, and anhysteretic remanent magnetization (ARM), are useful to characterize the rock magnetism of lavas. The 3 blocks from 2 sites of the middle aged lavas of the Shin-Fuji Volcano have extremely strong intensities ranging from 40 to 80 A/m and different rock magnetic character from the other samples with 5-25 A/m of a NRM intensity. The sampling sites are located near the lower margin of the lava flows. The strong NRM can be estimated by the precipitation of reduced iron in the lava flow, contaminated by growing vegetation.publishe
Whole - Rock Chemistry for Eruptive Products of Fuji Volcano, Central Japan: Summary of Aanalytical Data of 847 Samples.
No full textThe whole-rock chemistry for eruptive products of Fuji volcano is studied based on 847 newly
obtained analytical data. The volcanic activity of Fuji volcano consists of 6 stages which are proposed on
the basis of tephrochronology and whole-rock chemistry of eruptive products; they are the stage-1 (100 to 66ka), stage-2 (66 to 50 ka), stage-3 (50 to 25 ka), stage-4 (25 to18 ka), stage-5 (18 to 13 ka), stage-6 (13 to 4.5 ka), stage-7 (4.5 to 3.0 ka), stage-8 (3.0 to 2.0 ka) and stage-9 (2.0ka to Recent). The eruptive products
of stage-1 to stage-5 are members of the Ko - Fuji volcano and those of the stage-6 to stage-9 belong to the
Shin - Fuji volcano. The whole - rock chemistry of eruptive products were abruptly changed at about 18 ka;
the magmas erupted before 18 ka are called here the Ko - Fuji magmatic group and those after 18 ka the
Shin - Fuji magmatic group. The Shin - Fuji magmatic group is enriched in incompatible components such
as TiO₂, K₂O, P₂O₅, Rb, Ba, Zr and Nb, and shows higher ratios of Rb/Y, Ba/Y, Zr/Y and Nb/Y compared
with the Ko -Fuji magmatic group. The difference of both magmatic group cannot be explained by a simple
crystallization differentiation of the same parental magma, but it was produced by the melting of chemically
heterogeneous source mantle.departmental bulletin pape
KESALAHAN PENERJEMAHAN DRAMA JEPANG ICHI RITTORU NO NAMIDA KARYA MASANORI MURAKAMI
No full textThis study discusses the translation errors of the Indonesian subtitles from the Japanese drama Ichi Rittoru no Namida ‘One Liter Tears’ by Masanori Murakami, released at Fuji Terebi in 2005. There is no reference to similar study about the translation of oral dialogues of Japanese characters who were later translated into in Indonesian is of interest in this study. This study aims to identify the variety of Japanese drama Ichi Rittoru no Namida’s translation errors (subtitles). The formulation of the problem is examined with translation theory, types of translations and translation strategies. Furthermore, the data of this study are sentences or conversations in Japanese as the source language (SL) and Indonesian (subtitle) as the target language (TL) taken from episodes 1 to 6. The data are described using descriptive-qualitative methods. The results of this study are translation errors identified in diction choices, excessive use of words, grammatical errors, shifts in translation and errors due to cultural influences. Some examples of findings include the choice of diction like the word touzen translates to ‘legitimate’, excessive use of words such as the word gomen ne to ‘I am very sorry’, grammatical errors such as the phrase kondo no kusuri traced to ‘the medicine he is taking’, the translation shift as in the noun phrase todoufuken ga shiteishita ishi no shindansho it becomes ‘specified special health service’ and errors due to cultural influences such as the yoroshiku expression becomes ‘dependent on you’. Keywords: Ichi Rittoru no Namida, SL, TL, translation erro
富士山の地質と新富士溶岩の古地磁気
No full textapplication/pdfGeologic classification and distributions of the effusives of Fuji Volcano were com-piled mainly based on Tsuya (1968,1971) and the framework of geologic age by Miyaji (1988). The effusives can be classified into those of the Ko-Fuji and Shin-Fuji Volcanos, and that of the Shin-Fuji Volcano can be divided into 3,old, middle and young. The age of the boundary between the old and middle of Shin-Fuji Volcano is ca. 6300 years, and between middle and young is ca. 2200 years. The enormous amount of effusives of Fuji Volcano is related to the collision tectonics in central Japan, induced by motion of the Philip-pine Sea Plate. Paleomagnetic samples were collected from 11 sites of the old lavas and 3 sites of the middle aged lavas of the Shin-Fuji Volcano. Three oriented blocks were sampled from each site. The intensities of natural remanent magnetization (NRM) of most of the samples ranged from 5 to 25 A/m, and median destructive field (MDF) was 15-40mT. The direction of stepwise demagnetized NRM is stable and can be used for paleomagnetic studies. The positions of the virtual geomagnetic pole (VGP) are distributed around North Pole within latitudes higher than 60°N. VGP distributions are significantly different for the sites on the "same" lava. NRM intensities, MDF, anisotropy of magnetic susceptibility, and anhysteretic remanent magnetization (ARM), are useful to characterize the rock magnetism of lavas. The 3 blocks from 2 sites of the middle aged lavas of the Shin-Fuji Volcano have extremely strong intensities ranging from 40 to 80 A/m and different rock magnetic character from the other samples with 5-25 A/m of a NRM intensity. The sampling sites are located near the lower margin of the lava flows. The strong NRM can be estimated by the precipitation of reduced iron in the lava flow, contaminated by growing vegetation
Statistical analysis of Hydrographs of the Fuji Lakes (2nd Report)
No full textWe have studied the statistical property of the water-level of the Fuji lakes. In this paper, the author explained that the changes of the waterlevel had some continuity, that is, the changes were more continuous than the stochastic expectation, and the distribution of water-level between Motosu and Saiko has much correlation, but between Yamanaka and the others there is no correlation
STATISTICAL ADJUSTMENT OF HYDROGRAPH OF THE FUJI LAKES
No full textSome of the five lakes around Mt. Fuji, it is said, are connected with other. The author made scatter diagrams, control charts and time series diagrams by means of the rate of amplitude with statistical method, and proved that the western three lakes and the other two make respective groups and between these two groups there is no connection but there is much correlation among the western three but there are few between the easten two. These results coincide with the traditional legends
The Mt. Fuji submillimeter-wave telescope
No full textWe have developed a 1.2 m submillimeter-wave telescope at the summit of Mt. Fuji to survey emission lines of the neutral carbon atom (CI) toward the Milky Way. A superconductor-insulator-superconductor mixer receiver on the Nasmyth focus is used to observe the 492 GHz band in SSB and the 345 GHz band in DSB simultaneously. The receiver noise temperature is 300 K in SSB and 200 K in DSB for 492 and 345 GHz, respectively. The intermediate frequency frequency is 1.8–2.5 GHz. An acousto-optical spectrometer which has the total bandwidth of 0.9 GHz and 1024 channel outputs has also been developed. The telescope was installed at the summit of Mt. Fuji (alt. 3725 m) in July 1998. It has been remotely operated via a satellite communication system from Tokyo or Nobeyama. Atmospheric opacity at Mt. Fuji was 0.4–1.0 at 492 GHz during 30% of the time and 0.07–0.5 at 345 GHz during 60% of the time from November 1998 to February 1999. The system noise temperature was 1000–3000 K in SSB at 492 GHz and 500–2000 K in DSB at 345 GHz. We observed the CI (3P1–3P0: 492 GHz) and CO (J = 3–2: 345 GHz) emission lines from nearby molecular clouds with the beam size of 22 and 31, respectively. We describe the telescope system and report the performance obtained in the 1998 winter
The Mt. Fuji submillimeter-wave telescope
No full textWe have developed a 1.2 m submillimeter-wave telescope at the summit of Mt. Fuji to survey emission lines of the neutral carbon atom (CI) toward the Milky Way. A superconductor-insulator-superconductor mixer receiver on the Nasmyth focus is used to observe the 492 GHz band in SSB and the 345 GHz band in DSB simultaneously. The receiver noise temperature is 300 K in SSB and 200 K in DSB for 492 and 345 GHz, respectively. The intermediate frequency frequency is 1.8–2.5 GHz. An acousto-optical spectrometer which has the total bandwidth of 0.9 GHz and 1024 channel outputs has also been developed. The telescope was installed at the summit of Mt. Fuji (alt. 3725 m) in July 1998. It has been remotely operated via a satellite communication system from Tokyo or Nobeyama. Atmospheric opacity at Mt. Fuji was 0.4–1.0 at 492 GHz during 30% of the time and 0.07–0.5 at 345 GHz during 60% of the time from November 1998 to February 1999. The system noise temperature was 1000–3000 K in SSB at 492 GHz and 500–2000 K in DSB at 345 GHz. We observed the CI (3P1–3P0: 492 GHz) and CO (J = 3–2: 345 GHz) emission lines from nearby molecular clouds with the beam size of 22 and 31, respectively. We describe the telescope system and report the performance obtained in the 1998 winter.othe
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