Dehydration Melting Below the Undersaturated Transition Zone
Abstract
A reflector 70–130 km below the base of the transition zone beneath Tibet is observed in receiver functions and underside seismic reflections, at depths consistent with the transition of garnet to bridgmanite. Contrast in water storage capacity between the minerals of the Earth's transition zone and lower mantle suggests the possibility for dehydration melting at the top of the lower mantle. First-principles calculations combined with laboratory synthesis experiments constrain the mantle water capacity across the base of the transition zone and into the top of the lower mantle. Herein, we interpret the observed seismic signal as consistent with 3–4 vol % hydrous melt resulting from dehydration melting in the garnet to bridgmanite transition. Should seismic signals evident in downwelling region result from water contents representative of upper mantle water globally, this constrains the water stored in nominally anhydrous minerals in the mantle to <30% the mass of the surface oceans.
- Authors:
-
- The Ohio State Univ., Columbus, OH (United States)
- Westfälische Wilhelms‐Univ. Münster (Germany)
- Univ. of Bristol (United Kingdom)
- Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
- Univ. Paris-Saclay, Gif-sur-Yvette (France)
- Sorbonne Univ., Paris (France)
- Publication Date:
- Research Org.:
- Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
- Sponsoring Org.:
- National Science Foundation (NSF); USDOE National Nuclear Security Administration (NNSA)
- OSTI Identifier:
- 1604001
- Report Number(s):
- LA-UR-19-28369
Journal ID: ISSN 1525-2027
- Grant/Contract Number:
- 89233218CNA000001; EAR 1724693; EAR 14‐52545
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Geochemistry, Geophysics, Geosystems
- Additional Journal Information:
- Journal Volume: 21; Journal Issue: 2; Journal ID: ISSN 1525-2027
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; garnet; perovskite; ringwoodite; transition zone; melting; density functional theory
Citation Formats
Panero, Wendy R., Thomas, Christine, Myhill, Robert, Pigott, Jeffrey S., Raepsaet, C., and Bureau, H. Dehydration Melting Below the Undersaturated Transition Zone. United States: N. p., 2020.
Web. doi:10.1029/2019GC008712.
Panero, Wendy R., Thomas, Christine, Myhill, Robert, Pigott, Jeffrey S., Raepsaet, C., & Bureau, H. Dehydration Melting Below the Undersaturated Transition Zone. United States. https://doi.org/10.1029/2019GC008712
Panero, Wendy R., Thomas, Christine, Myhill, Robert, Pigott, Jeffrey S., Raepsaet, C., and Bureau, H. Tue .
"Dehydration Melting Below the Undersaturated Transition Zone". United States. https://doi.org/10.1029/2019GC008712. https://www.osti.gov/servlets/purl/1604001.
@article{osti_1604001,
title = {Dehydration Melting Below the Undersaturated Transition Zone},
author = {Panero, Wendy R. and Thomas, Christine and Myhill, Robert and Pigott, Jeffrey S. and Raepsaet, C. and Bureau, H.},
abstractNote = {A reflector 70–130 km below the base of the transition zone beneath Tibet is observed in receiver functions and underside seismic reflections, at depths consistent with the transition of garnet to bridgmanite. Contrast in water storage capacity between the minerals of the Earth's transition zone and lower mantle suggests the possibility for dehydration melting at the top of the lower mantle. First-principles calculations combined with laboratory synthesis experiments constrain the mantle water capacity across the base of the transition zone and into the top of the lower mantle. Herein, we interpret the observed seismic signal as consistent with 3–4 vol % hydrous melt resulting from dehydration melting in the garnet to bridgmanite transition. Should seismic signals evident in downwelling region result from water contents representative of upper mantle water globally, this constrains the water stored in nominally anhydrous minerals in the mantle to <30% the mass of the surface oceans.},
doi = {10.1029/2019GC008712},
journal = {Geochemistry, Geophysics, Geosystems},
number = 2,
volume = 21,
place = {United States},
year = {Tue Jan 14 00:00:00 EST 2020},
month = {Tue Jan 14 00:00:00 EST 2020}
}
Web of Science
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