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  • 1
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    In:  Eos, Trans., Am. Geophys. Un., Stuttgart, Pergamon, vol. 80, no. 50, pp. 605, 611, pp. 2249, (ISSN: 1340-4202)
    Publication Date: 1999
    Keywords: Earthquake ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Tectonics
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  • 2
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    In:  Seism. Res. Lett., Kunming, China, Elsevier, vol. 68, no. 6, pp. 931-943, pp. 2481, (ISSN: 1340-4202)
    Publication Date: 1997
    Keywords: Early warning systems (earthquakes, volcanic eruptions, tsunamis etc.) ; Real time earthquake monitoring ; Seismology ; CWB ; Location ; Magnitude ; SRL
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  • 3
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    Elsevier
    In:  Professional Paper, Open-File Rept., Urban Disaster Mitigation: The Role of Science and Technology, New York, Elsevier, vol. 8, no. 16, pp. 15-30, (ISBN 0080419208)
    Publication Date: 1995
    Keywords: Seismicity ; Earthquake hazard ; Statistical investigations ; Strong motions ; Spectrum ; Earthquake hazard ; Earthquake risk ; Earthquake engineering, engineering seismology
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  • 4
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    In:  Bull. Seism. Soc. Am., London, AGU, vol. 87, no. 5, pp. 1209-1219, pp. B02408, (ISSN: 1340-4202)
    Publication Date: 1997
    Keywords: Real time earthquake monitoring ; Strong motions ; Location ; Magnitude ; BSSA
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  • 5
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    In:  J. Geophys. Res., Moskva, EGS, vol. 75, no. 17, pp. 5729-5743, pp. L17304, (ISSN: 1340-4202)
    Publication Date: 1970
    Keywords: Source ; Seismology ; Spectrum ; Surface waves ; Hypocentral depth ; JGR
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  • 6
    ISSN: 1420-9136
    Keywords: Radon ; Groundwater ; Earthquakes ; Taiwan
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Radon (222Rn) concentration in geothermal waters and CO2-rich cold springwaters collected weekly in duplicate samples from four stations in northern Taiwan were measured from July 1980 to December 1983. Seven spike-like radon anomalies (increases of 2 to 3 times the standard deviation above the mean) were observed at three stations. Following every anomaly except one, an earthquake ofM L above 4.6 occurred within 4 to 51 days, at an epicentral distance 14 to 45 km, and at a focal depth of less than 10 km. The distribution of the earthquakes preceded by radon anomalies is skewed in certain directions from the radon stations; the radon stations seem to be insensitive to earthquakes occurring in the other directions. At the fourth station, near a volcanic area, much gas (mainly CO2) is discharged from the well, together with hot water. A very high concentration of radon was detected in the discharged gas; therefore trapping of gas in the water can result in anomalously high radon contents. According to limited measurements, the radon concentration in water appears to be undersaturated with respect to that in gas. This suggests that hot water is very susceptible to radon loss, and monitoring of radon in gas is more desirable.
    Type of Medium: Electronic Resource
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  • 7
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    In:  Tectonophys., Basel, Elsevier Science Publishers, vol. 333, no. 1-2, pp. 1-7, pp. 2519, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Review article ; Plate tectonics ; China ; Taiwan ; Kamchatka ; Japan ; Philippines ; Indonesia ; Papua ; New ; Guinea
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  • 8
    Publication Date: 2012-10-01
    Description: In this study, we use extreme value theory based on Gumbel-equation derivations to estimate the Gutenberg–Richter a and b parameters for Taiwan. Data are from the augmented, homogenized (in terms of moment magnitude), historic catalog for Taiwan. The island is divided into grids of 0.2° latitude by 0.2° longitude, and Gumbel type 1 statistical analysis is applied. The values of a and b are then used to determine the probability of large earthquakes ( M w ≥6.0) occurring at each grid. The results show two relatively high probability paths for large earthquakes, one extending from Hsinchu southward to Taichung, Chiayi, and Tainan in western Taiwan and the other from Ilan southward to Hualian and Taitung in eastern Taiwan, both of which are characterized by low b -values. It indicates that future earthquakes can be expected along these paths characterized by low b -values. Additionally, maximum peak ground acceleration and maximum peak ground velocity (determined from respective attenuation laws and a gridding regimen of 0.1° latitude by 0.1° longitude for Taiwan) follow similar paths to that of the low b -values.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
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  • 9
    Publication Date: 2013-02-07
    Description: The difference between S -wave and S -to- P -wave conversion ( S P phase) arrival times is enhanced with rectilinear motion detector filtering to describe alluvial-sediment thickness in the Kaohsiung–Pingtung (Kaoping) plains area. A more complete understanding of the underground structures of the Kaoping area is provided in this paper and explains why the surrounding regions in Taiwan experience more earthquakes than the Kaoping area. Data are based on seismic activity recorded by the portable array for numerical data acquisition (PANDA) for the period from 1995 to 1997. The difference between S -wave and S P -phase arrival times shows that the sedimentary layer is thicker along the west and southwest coasts. P -wave travel-time residuals, high-frequency attenuation parameters Kappa, and quality factor Q P , Q S , and coda waves confirm this result. We also determined the orientation of the Chaochou fault using the first motion of P -wave arrivals. To the east of the Chaochou fault, stress trends southeast–northwest, while to the west, it trends northeast–southwest. The change in stress trends east and west of Chaochou fault suggests the presence of a highly fluid accretionary wedge in the Kaoping area. The Chaochou fault forms a seismically active tectonic boundary with the uplift of the hanging wall leading to westward tilting of the basement of the Kaoping plains. We demonstrate that these features are the reason there are relatively few earthquakes in the Kaoping area. The presence of a highly fluid accretionary wedge is indicated by a thick alluvial layer in the west and southwest Kaoping coasts; the Peikung High acts as the indenter that may allow seismic energy to escape and reduce the number of earthquakes in the region. Online Material: Figures illustrating calculations of Kappa, Q c , P - and S -wave spectra, Q P , and Q S from ground-motion data.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
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  • 10
    Publication Date: 2016-01-27
    Description: The purpose of this study is to assess seismic hazards in the 57 administration districts of the Chianan area (Chiayi County, Chiayi City, and Tainan City), Taiwan, in the form of ShakeMaps, as well as to estimate potential human fatalities from scenario earthquakes on the three type I active faults in this area. The resultant ShakeMap patterns of maximum ground motion show two regions with high modified Mercalli intensity (MMI; greater than IX). One is in the Chiayi area around Minsyong, Dalin, and Meishan due to presence of the Meishan fault and large site amplification factors. The other is in the Tainan area around Jiali, Madou, Siaying, Syuejia, Jiangjyun, and Yanshuei. The projected probabilities in 10, 30, and 50 yr periods with seismic intensity exceeding MMI VIII in these areas are greater than 45%, 80%, and 95%, respectively. Furthermore, from the distribution of probabilities, high values of greater than 95% over a 10 yr period with seismic intensity corresponding to Central Weather Bureau intensity V and MMI VI are found in central and northern Chiayi and northern Tainan. Finally, from estimation of potential human fatalities for scenario earthquakes on three active faults in Chianan area, it is noted that potential fatalities increase rapidly for people above age 45. Total fatalities reach high peaks in two age groups, ages 60–64 and 75–79, respectively, from scenario earthquakes on the Meishan and Chukou faults. On the other hand, total fatalities peak at ages 55–64 in the case of Hsinhua fault; this is probably because more people in this age group live in the nearby densely populated urban areas (〉5000 persons/km 2 ) such as the Yongkang District. We urge the local and central governments to pay special attention to seismic-hazard mitigation in this urbanized area, with its large number of old buildings. Online Material: Maps of probabilities of exceeding Central Weather Bureau intensity (CWBI) V, VI, and VII and modified Mercalli intensity (MMI) VI and VII of ground shaking over 10, 30, and 50 yr periods.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
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