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  • 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations  (1)
  • Accumulation rate, alkenone C37; Accumulation rate, total organic carbon; AGE; Alkenone, C37 normalized to total organic carbon; Alkenone, unsaturation index UK37; Calcium carbonate; Carbon, organic, total; Carbon/Nitrogen ratio; Density, dry bulk; DEPTH, sediment/rock; KT05-7; KT05-7_PC-02; Nitrogen, total; PC; PC-02; Period; Piston corer; Sample code/label; Sea surface temperature, annual mean; Sedimentation rate; Tansei Maru; West Pacific Ocean  (1)
  • 2005-2009  (2)
  • 1980-1984
Collection
Keywords
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Years
Year
  • 1
    Publication Date: 2019-11-04
    Description: Campi Flegrei is a unique volcanic region located near Naples, Italy. Anomalous crustal movements at Pozzuoli in Campi Flegrei have been documented since the Roman period. The movements were gradual and have continued to the present, occasionally accompanying swarms of local earthquakes and volcanic eruptions. Generally the movements proceed with low seismicity. After the 1538 eruption of Monte Nuovo, Pozzuoli had subsided monotonously, but it changed to uplift abruptly in 1969. The uplift accelerated in 1983 and 1984 reaching more than 2 m, and thereafter began to subside. Many discussions of this event have been published. In Japan, we have examples of deformations similar to those at Campi Flegrei, mainly in volcanic areas, and rarely in non-volcanic areas. The former includes Iwojima, Miyakejima and Aira caldera while the latter is represented by Cape Omaezaki. Iwojima is a volcano island, and its secular uplifts since the 18th century are recognized as an unusual event. Miyakejima volcano and Aira caldera exhibited anomalous movements with low seismicity after their eruptions. Cape Omaezaki is not situated in volcanic zone but near a subduction zone, and gradually and continuously subsides as a precursor to a large earthquake. In such cases as Campi Flegrei and the Japanese localities, we would question whether the deformations are accompanied by normal seismicity or low seismicity. To examine quantitatively the relationship between seismicity and related deformation, seismic efficiency is generally useful. The crustal deformations in all the regions cited above are characterized by exceptionally low seismic efficiencies. In the present paper, the deformations at Pozzuoli and Iwojima are mainly described and a comparative discussion among these and other localities in Japan is supplemented. It is concluded that such anomalous phenomena in volcanic areas are attributable to peculiar rheological aspects of the material composing the local upper crust, and the deformation in a non-volcanic area is of tectonic origin.
    Description: Published
    Description: JCR Journal
    Description: open
    Keywords: crustal movements ; low seismic efficiency ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations ; 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 391986 bytes
    Format: application/pdf
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  • 2
    Publication Date: 2024-01-25
    Keywords: Accumulation rate, alkenone C37; Accumulation rate, total organic carbon; AGE; Alkenone, C37 normalized to total organic carbon; Alkenone, unsaturation index UK37; Calcium carbonate; Carbon, organic, total; Carbon/Nitrogen ratio; Density, dry bulk; DEPTH, sediment/rock; KT05-7; KT05-7_PC-02; Nitrogen, total; PC; PC-02; Period; Piston corer; Sample code/label; Sea surface temperature, annual mean; Sedimentation rate; Tansei Maru; West Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 1013 data points
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