Initial results from WING, the continuous GPS network in the western Pacific area

To investigate tectonic deformation in the western Pacific, a continuous GPS tracking network has been established, and named the Western Pacific Integrated Network of GPS (WING). Between 1995 and March 1997 we establised ten new sites. Data for the period July 1995 to October 1996 were analyzed, to...

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Published inGeophysical research letters Vol. 25; no. 3; pp. 369 - 372
Main Authors Kato, Teruyuki, Kotake, Yoshiko, Nakao, Shigeru, Beavan, John, Hirahara, Kazuro, Okada, Masami, Hoshiba, Mitsuyuki, Kamigaichi, Osamu, Feir, Renato B., Park, Pil Ho, Gerasimenko, Mikhail D., Kasahara, Minoru
Format Journal Article
LanguageEnglish
Published Blackwell Publishing Ltd 01.02.1998
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Abstract To investigate tectonic deformation in the western Pacific, a continuous GPS tracking network has been established, and named the Western Pacific Integrated Network of GPS (WING). Between 1995 and March 1997 we establised ten new sites. Data for the period July 1995 to October 1996 were analyzed, together with data from International GPS Service for Geodynamics (IGS) global sites, to estimate daily coordinates. A fiducial‐free approach was used to obtain the most accurate baseline estimates. To fix the estimated coordinates to the terrestrial reference frame, the Tsukuba IGS site is assumed to be moving westward relative to the stable Eurasian continent at ∼2 cm/yr according to Heki's [1996] estimate. We find that: (1) velocities of sites well within oceanic plates are in good agreement with rigid plate motion models; (2) sites close to plate boundaries are all affected by the deformation at those boundaries, among which back‐arc rifting (spreading) is clearly visible at the Mariana and Okinawa troughs; (3) sites in eastern Asia are moving east to east‐southeast relative to the stable Eurasian continent, suggesting long distance effects of the northward collision of India with Asia.
AbstractList To investigate tectonic deformation in the western Pacific, a continuous GPS tracking network has been established, and named the Western Pacific Integrated Network of GPS (WING). Between 1995 and March 1997 we establised ten new sites. Data for the period July 1995 to October 1996 were analyzed, together with data from International GPS Service for Geodynamics (IGS) global sites, to estimate daily coordinates. A fiducial‐free approach was used to obtain the most accurate baseline estimates. To fix the estimated coordinates to the terrestrial reference frame, the Tsukuba IGS site is assumed to be moving westward relative to the stable Eurasian continent at ∼2 cm/yr according to Heki's [1996] estimate. We find that: (1) velocities of sites well within oceanic plates are in good agreement with rigid plate motion models; (2) sites close to plate boundaries are all affected by the deformation at those boundaries, among which back‐arc rifting (spreading) is clearly visible at the Mariana and Okinawa troughs; (3) sites in eastern Asia are moving east to east‐southeast relative to the stable Eurasian continent, suggesting long distance effects of the northward collision of India with Asia.
To investigate tectonic deformation in the western Pacific, a continuous GPS tracking network has been established, and named the Western Pacific Integrated Network of GPS (WING). Between 1995 and March 1997 we established ten new sites. Data for the period July 1995 to October 1996 were analyzed, together with data from International GPS Service for Geodynamics (IGS) global sites, to estimate daily coordinates. A fiducial-free approach was used to obtain the most accurate baseline estimates. To fix the estimated coordinates to the terrestrial reference frame, the Tsukuba IGS site is assumed to be moving westward relative to the stable Eurasian continent at similar to 2 cm/yr according to Heki's [1996] estimate. We find that: (1) velocities of sites well within oceanic plates are in good agreement with rigid plate motion models; (2) sites close to plate boundaries are all affected by the deformation at those boundaries, among which back-arc rifting (spreading) is clearly visible at the Mariana and Okinawa troughs; (3) sites in eastern Asia are moving east to east-southeast relative to the stable Eurasian continent, suggesting long distance effects of the northward collision of India with Asia.
To investigate tectonic deformation in the western Pacific, a continuous GPS tracking network has been established, and named the Western Pacific Integrated Network of GPS (WING). Between 1995 and March 1997 we establised ten new sites. Data for the period July 1995 to October 1996 were analyzed, together with data from International GPS Service for Geodynamics (IGS) global sites, to estimate daily coordinates. A fiducial‐free approach was used to obtain the most accurate baseline estimates. To fix the estimated coordinates to the terrestrial reference frame, the Tsukuba IGS site is assumed to be moving westward relative to the stable Eurasian continent at ∼2 cm/yr according to Heki 's [1996] estimate. We find that: (1) velocities of sites well within oceanic plates are in good agreement with rigid plate motion models; (2) sites close to plate boundaries are all affected by the deformation at those boundaries, among which back‐arc rifting (spreading) is clearly visible at the Mariana and Okinawa troughs; (3) sites in eastern Asia are moving east to east‐southeast relative to the stable Eurasian continent, suggesting long distance effects of the northward collision of India with Asia.
Author Hirahara, Kazuro
Park, Pil Ho
Gerasimenko, Mikhail D.
Beavan, John
Okada, Masami
Kotake, Yoshiko
Kamigaichi, Osamu
Kasahara, Minoru
Hoshiba, Mitsuyuki
Kato, Teruyuki
Nakao, Shigeru
Feir, Renato B.
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  surname: Kotake
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  organization: Earthquake Research Institute, University of Tokyo, Tokyo, Japan
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  organization: Earthquake Research Institute, University of Tokyo, Tokyo, Japan
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  organization: Institute of Geological and Nuclear Sciences, Lower Hutt, New Zealand
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  organization: Graduate School of Science, Nagoya University, Nagoya, Japan
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  surname: Feir
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  organization: Coast and Geodetic Survey Department, NAMRIA, Manila, Philippines
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  givenname: Pil Ho
  surname: Park
  fullname: Park, Pil Ho
  organization: Korea Astronomy Observatory, Daejeon, Korea
– sequence: 11
  givenname: Mikhail D.
  surname: Gerasimenko
  fullname: Gerasimenko, Mikhail D.
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  organization: Faculty of Science, Hokkaido University, Sapporo, Japan
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References_xml – reference: Argus, D.R. Gordon, No-net rotation model of current plate velocities incorporating plate motion model NUVEL-1, Geophys. Res. Lett., 18, 2039-2042, 1991
– reference: Weissel, J. K.R. N. Anderson, Is there a Caroline plate? Earth Planet. Sci. Lett., 41, 143-158, 1978
– reference: Bernese GPS Software Version 4.0, M. RothacherL. Mervert, Astronomical Institute, University of Berne, 1996
– reference: Larson, K.J. T. FreymuellerS. Philipsen, Global plate velocities from the Global Positioning System, J. Geophys. Res., 102, 9961-9981, 1997
– reference: Seno, T.S. SteinA. E. Gripp, A model for the motion of the Philippine Sea plate consistent with NUVEL- 1 and geophysical data, J. Geophys. Res., 98, 17941-17948, 1993
– reference: Kato, T.Y. KotakeT. ChachinY. IimuraS. MiyazakiT. KanazawaK. Suyehiro, An estimate of the Philippine Sea plate motion derived from the Global Positioning System observation at Okino Torishima, Japan, J. Geod. Soc. Japan, 42, 233-243, 1996
– reference: CamposJ. R. MadariagaC. Scholz, Faulting process of the August 8, 1993, Guam earthquake: A thrust event in an otherwise weakly coupled subduction zone, J. Geophys. Res., 101, 17581-17596, 1996
– reference: Scholz, C. H.J. Campos, On the mechanism of seismic decoupling and back arc spreading at subduction zones, J. Geophys. Res., 100, 22103-22115, 1995
– reference: Sibuet, J.-C.J. LetouzeyF. BarbierJ. CharvetJ.-P. FoucherT. W. C. HildeM. KimuraC. Ling-YunB. MarssetC. MullerJ.-F. Stephan, Backarc extension in the Okinawa Trough, J. Geophys. Res., 92, 14041-14063, 1987
– reference: Zonenshain, L. P.L. A. Savostin, Geodynamics of the Baikal rift zone and plate tectonics of Asia, Tectonophysics, 76, 1-45, 1981
– reference: Kato, T., Recent global and regional studies using GPS - A brief overview -, J. Geod. Soc. Japan, 38, 329-348, 1993
– reference: Heki, K.Y. TakahashiT. Kondo, Contraction of northeastern Japan: evidence from horizontal displacement of a Japanese station in global very long baseline interferometry networks, Tectonophysics, 181, 113-122, 1990
– reference: Bevis, M.F. W. TaylorB. E. SchutzJ. RecyB. L. IsacksS. HeluR. SinghE. KendrickJ. StowellB. TaylorandS. Calmant, Geodetic observations of very rapid convergence and back-arc extension at the Tonga arc, Nature, 374, 249-251, 1996
– reference: Hussong, D. M.S. Uyeda, Tectonic processes and the history of the Mariana arc: A synthesis of the results of deep sea drilling project LEG 60, Initial Reports of the Deep Sea Drilling Project, 60, 909-929, 1981
– reference: Wessel, P.W. H. F. Smith, Free software helps map and display data, EOS Trans. AGU, 72, 441, 445-446, 1991
– reference: Ranken, B.R. K. CardwellD. E. Karig, Kinematics of the Philippine Sea Plate, Tectonics, 3, 555-575, 1984
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Snippet To investigate tectonic deformation in the western Pacific, a continuous GPS tracking network has been established, and named the Western Pacific Integrated...
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SubjectTerms Marine
Title Initial results from WING, the continuous GPS network in the western Pacific area
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