Japão milagre econômico e sacrifício social

Vale, Glaúcia Maria Vasconcellos

doi:10.1590/s0034-75901992000200006

Rev. adm. empres.

1992

DOI: 10.1590/s0034-75901992000200006

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Japão milagre econômico e sacrifício social

Glaúcia Maria Vasconcellos Vale¹

Abstract: A autora analisa a performance da economia japonesa, através de alguns "indicadores de sucesso" de uso corrente: eficiência estática, eficiência dinâmica, taxa de crescimento da renda nacional, satisfação do consumidor e perfil de renda. Faz uma minuciosa incursão no terreno da organização industrial e no ambiente empresarial do país, demonstrando os pontos vulneráveis do chamado "milagre japonês"

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2006

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The upper Pliocene diatom zone and fission-track age of the upper Koetoi Formation around the Sarobetsu anticline, northern Hokkaido

健一¹,

文雄²,

寛人³

et al. 2006

Jour. Geol. Soc. Japan

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We carried out fossil diatom analysis and fission-track dating of the upper Koetoi Formation, which is distributed in the western limb of the Sarobetsu anticline in the western part of the Horonobe area, northern Hokkaido. A mudstone sample collected from the upper Koetoi Formation contains abundant autochthonous diatoms which can clearly be correlated with the Neodenticula koizumii Zone. The assemblage includes N. seminae, which has a first appearance age of. Ma. A zircon FT age obtained from an interbeded volcanic ash is. . Ma. This FT result gives a precise depositional age for the upper Koetoi Formation in the area surveyed, and is consistent with the results of the diatom fossil analysis. These results indicate that the depositional age of the upper Koetoi Formation is about. Ma. Considering previous chronological work and our results, the age of the boundary between the Koetoi and the Yuchi Formations in the western part of the Horonobe area is younger than about. Ma, which is at least million years younger than that of the same boundary in the eastern part. This implies westward depositional migration of the Koetoi and Yuchi Formations, and a diachronous relationship between the eastern and the western parts. These geochronological constraints from diatom fossils and FT data further suggest that the period of incipient active tectonism, which formed complex anticlinal and synclinal structures in this area is younger than about. Ma. The volcanic ash layer in the upper Koetoi Formation contains characteristic zircon crystals with unusually high uranium contents ppm , and may become a useful marker bed in this area.

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The upper Pliocene diatom zone and fission-track age of the upper Koetoi Formation around the Sarobetsu anticline, northern Hokkaido

健一¹,

文雄²,

寛人³

et al. 2006

Jour. Geol. Soc. Japan

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Three-dimensional distribution and hydrogeological properties of the Omagari Fault in the Horonobe area, northern Hokkaido, Japan

Ishii

Yasue

Tanaka

et al. 2006

Jour. Geol. Soc. Japan

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We investigated the geological structure and hydrogeological properties of the Omagari Fault in Neogene siliceous sedimentary rocks of the Horonobe area, northern Hokkaido, by geological mapping, borehole investigations, reflection seismic survey, and audio-frequency magnetotelluric survey. As a result of the investigation, the-D distribution of the Fault was clarified and the following were shown. In addition, the magnetotelluric survey in particular was effective for mapping of the-D distribution and hydrogeological properties of the fault. The Omagari Fault has a fault zone, about m wide, that consists mainly of the damage zone, and has a permeable structure. The magnetotelluric survey shows several high-resistivity zones, one of which corresponds to the Omagari Fault inferred from the reflection seismic surveys. The high resistivity zones are correlative with the concentration zones of low-saline water, which suggests infiltration of ground water through the permeable Omagari Fault zone. The Omagari Fault over-steps at the earth surface and at the same time is converging in subsurface zones.

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Japão milagre econômico e sacrifício social

Cited by 2 publications

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The upper Pliocene diatom zone and fission-track age of the upper Koetoi Formation around the Sarobetsu anticline, northern Hokkaido

The upper Pliocene diatom zone and fission-track age of the upper Koetoi Formation around the Sarobetsu anticline, northern Hokkaido

Three-dimensional distribution and hydrogeological properties of the Omagari Fault in the Horonobe area, northern Hokkaido, Japan

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