Slab Transport of Fluids to Deep Focus Earthquake Depths—Thermal Modeling Constraints and Evidence From Diamonds
Author:
Affiliation:
1. Earth and Planets Laboratory Carnegie Institution for Science Washington DC USA
2. Department of Earth and Atmospheric Sciences University of Alberta Edmonton AB Canada
Funder
National Science Foundation
Carnegie Institution for Science
University of Alberta
Publisher
American Geophysical Union (AGU)
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020AV000304
Reference183 articles.
1. The role of serpentinites in cycling of carbon and sulfur: Seafloor serpentinization and subduction metamorphism
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4. Tetragonal almandine pyrope phase (TAPP): retrograde Mg-perovskite from subducted oceanic crust?
5. The relationship of intermediate- and deep-focus seismicity to the hydration and dehydration of subducting slabs
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