The effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle

Lunar cumulate mantle overturn and the subsequent upwelling of overturned mantle cumulates provide a potential framework for understanding the first-order thermochemical evolution of the Moon. Upwelling of ilmenite-bearing cumulates (IBCs) after the overturn has a dominant influence on the dynamics...

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Main Authors: Zhang, Nan, Dygert, N., Liang, Y., Parmentier, E.
Format: Journal Article
Published: American Geophysical Union 2017
Online Access:http://hdl.handle.net/20.500.11937/68141
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author Zhang, Nan
Dygert, N.
Liang, Y.
Parmentier, E.
author_facet Zhang, Nan
Dygert, N.
Liang, Y.
Parmentier, E.
author_sort Zhang, Nan
building Curtin Institutional Repository
collection Online Access
description Lunar cumulate mantle overturn and the subsequent upwelling of overturned mantle cumulates provide a potential framework for understanding the first-order thermochemical evolution of the Moon. Upwelling of ilmenite-bearing cumulates (IBCs) after the overturn has a dominant influence on the dynamics and long-term thermal evolution of the lunar mantle. An important parameter determining the stability and convective behavior of the IBC is its viscosity, which was recently constrained through rock deformation experiments. To examine the effect of IBC viscosity on the upwelling of overturned lunar cumulate mantle, here we conduct three-dimensional mantle convection models with an evolving core superposed by an IBC-rich layer, which resulted from mantle overturn after magma ocean solidification. Our modeling shows that a reduction of mantle viscosity by 1 order of magnitude, due to the presence of ilmenite, can dramatically change convective planform and long-term lunar mantle evolution. Our model results suggest a relatively stable partially molten IBC layer that has surrounded the lunar core to the present day.
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spelling curtin-20.500.11937-681412018-10-01T03:04:16Z The effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle Zhang, Nan Dygert, N. Liang, Y. Parmentier, E. Lunar cumulate mantle overturn and the subsequent upwelling of overturned mantle cumulates provide a potential framework for understanding the first-order thermochemical evolution of the Moon. Upwelling of ilmenite-bearing cumulates (IBCs) after the overturn has a dominant influence on the dynamics and long-term thermal evolution of the lunar mantle. An important parameter determining the stability and convective behavior of the IBC is its viscosity, which was recently constrained through rock deformation experiments. To examine the effect of IBC viscosity on the upwelling of overturned lunar cumulate mantle, here we conduct three-dimensional mantle convection models with an evolving core superposed by an IBC-rich layer, which resulted from mantle overturn after magma ocean solidification. Our modeling shows that a reduction of mantle viscosity by 1 order of magnitude, due to the presence of ilmenite, can dramatically change convective planform and long-term lunar mantle evolution. Our model results suggest a relatively stable partially molten IBC layer that has surrounded the lunar core to the present day. 2017 Journal Article http://hdl.handle.net/20.500.11937/68141 10.1002/2017GL073702 American Geophysical Union fulltext
spellingShingle Zhang, Nan
Dygert, N.
Liang, Y.
Parmentier, E.
The effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle
title The effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle
title_full The effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle
title_fullStr The effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle
title_full_unstemmed The effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle
title_short The effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle
title_sort effect of ilmenite viscosity on the dynamics and evolution of an overturned lunar cumulate mantle
url http://hdl.handle.net/20.500.11937/68141