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Session
  • Presentation | DI22A: Mantle Convection, Phase Transitions, and Evolution of Earth and Other Rocky Planets II Oral
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  • DI22A-03: Elasticity of Fe,Al,Mg,Ti-bearing Davemaoite Explains Lower Mantle Seismic Heterogeneities (invited)
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  • Location Icon348-349
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Author(s):
Jin Zhang, Texas A&M University College Station (First Author, Presenting Author)
Wen-Yi Zhou, University of New Mexico, Earth & Planetary Sciences
Ming Hao, University of New Mexico, Earth & Planetary Sciences
Wenhao Su, Texas A&M University College Station
Taehyun Kim, Arizona State University
Sibo Chen, Stony Brook University
Sang-Heon Dan Shim, Arizona State University
Phuong Nguyen, University of Hawaii at Manoa
Dongzhou Zhang, Caltech-Seismolab
Katherine Armstrong, Lawrence Berkeley National Lab


Davemaoite in MORB is seismically extremely slow, making it an excellent mineralogic candidate for various lower mantle heterogeneities that are important for the Earth's evolution, including and not limited to ULVZs and LLSVPs.



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