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Title: 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:
 [1];  [2];  [3]; ORCiD logo [4];  [5];  [6]
  1. The Ohio State Univ., Columbus, OH (United States)
  2. Westfälische Wilhelms‐Univ. Münster (Germany)
  3. Univ. of Bristol (United Kingdom)
  4. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
  5. Univ. Paris-Saclay, Gif-sur-Yvette (France)
  6. 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}
}

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