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  • 1
    Publication Date: 2024-04-20
    Description: To examine the temperature impact on the DPG signals related to internal motions, four Cox-Webb differential pressure gauges (DPGs) fixed on the ocean bottom and a high-resolution temperature sensor (T-sensor) 13 m above the seafloor as a square-kilometer array deployed offshore eastern Taiwan facing the open Pacific Ocean. The DPGs and T-sensor were built by the Institute of Earth Sciences of Academia Sinica and Royal Netherlands Institute for Sea Research (NIOZ), respectively. In addition, a Nortek AquaDopp acoustic current meter with pressure sensor was attached on the same vertical string with the T-sensor at 2936 m. The multiple instruments in the array were located at depths between 3000 and 3200 m with inter-station horizontal distances ranging from about 300 m to 1 km. The time series data with 2 mHz sampling rate in ASCII format were used to study propagation of the deep-sea internal waves between September 2017 and April 2018. Fifteen events of the internal motions were selected by T-sensor-DPG correlation coefficient 〉 0.7 at every DPG in a 3-day time window that is shifted in time by 1 day. The propagating direction and apparent horizontal phase speed of the internal waves can be estimated by the DPG data using array analysis methods.
    Keywords: MULT; Multiple investigations; Taiwan; Taiwan_SEcoast
    Type: Dataset
    Format: application/zip, 644.1 kBytes
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © The Authors, 2009. This article is posted here by permission of John Wiley & Sons for personal use, not for redistribution. The definitive version was published in Geophysical Journal International 179 (2009): 1859-1869, doi:10.1111/j.1365-246X.2009.04391.x.
    Description: A broad-band ocean-bottom seismometer (OBS) deployed ~180 km east of Taiwan provides a first glimpse into the upper mantle beneath the westernmost section of the Philippine Sea or the Huatung basin (HB). We measured interstation phase velocities of Rayleigh waves between the OBS and stations on the eastern coast of Taiwan. The phase velocities show smooth variations from 3.8 to 3.9 km s−1 for periods of 25–40 s. In this short period range, phase velocities are comparable to those characterizing the 15–30 Ma Parece-Vela basin of the Philippine Sea. Modelling of the finite-frequency effect proves the validity of the measurement for the average HB. The shear-wave velocity models inverted from the 25 to 40 s dispersion show a velocity at lithospheric depths about 0.1 km s−1 lower than that of the west Philippine Sea, which agrees with the age effect derived from the Pacific pure-path model. Inversions incorporating the less reliable data above 40 s yield a shear velocity 〈4.0 km s−1 below 150 km, an unrealistic value even for a hotspot plume environment. The seismological evidence, together with the correlation in seafloor depth, suggests that the HB and the Parece-Vela basin may have a similar age. This is at odds with the previous geochronological study suggesting an early-Cretaceous age for the HB. Thermal rejuvenation of the lithosphere was examined as a potential solution to reconciling the two age models.
    Description: The research is supported by the National Science Council, Taiwan, Republic of China, under grant NSC 96–2745-M-001–005.
    Keywords: Surface waves and free oscillations ; Wave propagation ; Continental margins: convergent ; Dynamics of lithosphere and mantle
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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