High‐frequency waves guided by the subducted plates underneath Taiwan and their association with seismic intensity anomalies

No abstract is available for this paper.

• Publication year

  2011

• Venue

  Journal of Geophysical Research: Solid Earth

• Publication date

  2011-12-01

• Fields of study

  Geology

• Identifiers
  DOI 10.1002/jgrb.50071
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

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  2009influential reference
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  2008cited by this paper
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  2003influential reference
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  2002cited by this paper
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  2000influential reference
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  1996influential reference
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  1996cited by this paper
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  1995cited by this paper
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  1990influential reference
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  1986cited by this paper
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  1986cited by this paper
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  1985influential reference
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  1985cited by this paper
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  1983cited by this paper
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  1981cited by this paper
• Paleogeographic origins of the Miocene East Taiwan Ophiolite

  1981cited by this paper
• Plate Convergence and Accretion in Taiwan-Luzon Region

  1978cited by this paper
• THE INSTANTANEOUS ROTATION VECTOR OF THE PHILIPPINE SEA PLATE RELATIVE TO THE EURASIAN PLATE

  1977cited by this paper
• A model not requiring continuous lithosphere for anomalous high-frequency arrivals from deep-focus South American earthquakes

  1974cited by this paper
• High Frequency Shear Waves Guided by a Continuous Lithosphere Descending beneath western South America

  1973cited by this paper
• Propagation of seismic waves through and beneath the lithosphere that descends under the Tonga Island Arc

  1972cited by this paper
• Anomalies in Seismic Wave Velocity and Attenuation Associated with a Deep Earthquake Zone(2)

  1967cited by this paper
• Regional Differences in Absorption of Seismic Waves in the Upper Mantle as Inferred from Abnomal Distributions of Seismic Intensities

  1966influential reference
• On the Variation of General Circulation in 1901-1940

  1959cited by this paper

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  2024cites this paper
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  2024influential citation
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