Magnitude and symmetry of seismic anisotropy in mica‐ and amphibole‐bearing metamorphic rocks and implications for tectonic interpretation of seismic data from the southeast Tibetan Plateau

Author:

Ji Shaocheng1,Shao Tongbin1,Michibayashi Katsuyoshi2,Oya Shoma2,Satsukawa Takako3ORCID,Wang Qian4,Zhao Weihua5,Salisbury Matthew H.6

Affiliation:

1. Département des Génies Civil, Géologique et des MinesÉcole Polytechnique de Montréal Montréal Québec Canada

2. Institute of GeosciencesShizuoka University Shizuoka Japan

3. ARC Centre of Excellence for Core to Crust Fluid Systems, GEMOC, Department of Earth and Planetary SciencesMacquarie University Sydney New South Wales Australia

4. Guangzhou Institute of GeochemistryChinese Academy of Sciences Guangzhou China

5. Institute of GeomechanicsChinese Academy of Geological Sciences Beijing China

6. Geological Survey of Canada‐AtlanticBedford Institute of Oceanography Dartmouth Nova Scotia Canada

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

American Geophysical Union (AGU)

Subject

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

Reference144 articles.

1. Geometry, kinematics, and regional significance of the Chong Shan shear zone, Eastern Himalayan Syntaxis, Yunnan, China

2. The elastic properties of rock‐forming minerals, II: Layered silicates;Aleksandrov K. S.;Izv. Acad. Sci. USSR, Geophys. Ser.,1961

3. Velocities of elastic waves in minerals at atmospheric pressure and increasing precision of elastic constants by means of EVM [in Russian];Aleksandrov K. S.;Izv. Acad. Sci. USSR, Geol. Ser.,1974

4. Elastic properties, fabric and seismic anisotropy of amphibolites and their contribution to the lower crust reflectivity

5. Seismic anisotropy and shear-wave splitting in lower-crustal and upper-mantle rocks from the Ivrea Zone—experimental and calculated data

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