Constraining Sedimentary Structure Using Frequency-Dependent P Wave Particle Motion: A Case Study of the Songliao Basin in NE China

Author:

Bao Yifei12,Niu Fenglin12ORCID

Affiliation:

1. State Key Laboratory of Petroleum Resource and Prospecting, and Unconventional Gas Institute; China University of Petroleum at Beijing; Beijing China

2. Department of Earth Science; Rice University; Houston TX USA

Funder

National Sleep Foundation

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference27 articles.

1. Inversion of receiver functions without deconvolution-Application to the Indian craton;Bodin;Geophysical Journal International,2014

2. Rayleigh wave particle motion and crustal structure;Boore;Bulletin of the Seismological Society of America,1969

3. Empirical relations between elastic wavespeeds and density in the Earth's crust;Brocher;Bulletin of the Seismological Society of America,2005

4. Relationships between compressional-wave and shear-wave velocities in clastic silicate rocks;Castagna;Geophysics,1985

5. Joint inversion of receiver functions and surface waves with enhanced preconditioning on densely distributed CNDSN stations: Crustal and upper mantle structure beneath China;Chen;Journal of Geophysical Research: Solid Earth,2016

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