Hydrostatic Dehydration Fabrics of Antigorite at High Pressure and High Temperature: Implications for Trench Parallel Seismic Anisotropy at Convergent Plate Boundaries-Reference-Cited by-同舟云学术

Hydrostatic Dehydration Fabrics of Antigorite at High Pressure and High Temperature: Implications for Trench Parallel Seismic Anisotropy at Convergent Plate Boundaries

Published:2021-09 Issue:9 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Liu W. L.¹²,Qi H. W.¹,Zhang J. F.¹^ORCID,Wu X.¹,Li J. F.³,Zhao R.¹,Wang Y. F.¹^ORCID,Jin Z. M.¹^ORCID

Affiliation:

1. State Key Laboratory of Geological Processes and Mineral Resources School of Earth Sciences China University of Geosciences Wuhan China

2. China University of Geosciences Institute of Geophysics & Geomatics Wuhan China

3. State Key Laboratory of Isotope Geochemistry Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou 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

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB021671

Reference76 articles.

1. The elastic constants of San Carlos olivine to 17 GPa

2. Seismic signatures of a hydrated mantle wedge from antigorite crystal-preferred orientation (CPO)

3. The elastic constants of an aluminous orthopyroxene to 12.5 GPa

4. Interplay between Fluid Extraction Mechanisms and Antigorite Dehydration Reactions (Val Malenco, Italian Alps)

5. Devolatilization-generated fluid pressure and deformation-propagated fluid flow during prograde regional metamorphism

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