Seismic Azimuthal Anisotropy for the Southeastern Tibetan Plateau Extracted by Wave Gradiometry Analysis

Author:

Cao Feihuang12ORCID,Liang Chuntao12ORCID,Zhou Lu2,Zhu Jieshou2

Affiliation:

1. State Key Laboratory of Geohazard Prevention and Geoenvironment Protection Chengdu University of Technology Chengdu China

2. Key Laboratory of Earth Exploration and Information Techniques of the China Ministry of Education Chengdu China

Funder

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

Reference111 articles.

1. Complex, multilayered azimuthal anisotropy beneath Tibet: evidence for co-existing channel flow and pure-shear crustal thickening

2. Emeishan large igneous province (SW China) and the mantle-plume up-doming hypothesis

3. Emeishan large igneous province, SW China

4. Anisotropy in deeper parts of the Earth[M]//Seismic anisotropy in the earth;Babuska V.;Springer Netherlands,1991

5. Possible forms of seismic anisotropy of the uppermost mantle under oceans[J];Backus G. E.;Journal of Geophysical Research,1965

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