11 Structural Geology (Posters)

Sunday, 19 March 2017
8:00 AM - 12:00 PM
Urban, 17th Floor

GRAIN SIZE DEPENDENCE OF PLASTIC STRENGTH OF MAGNESITE

Paper number: 11-7
Program: Technical Sessions
Time: 8:00 AM – 12:00 PM

Authors

Abstract

Magnesite is a carbonate mineral formed by alteration of olivine-rich peridotites by CO2-bearing fluids in subducting slabs. Magnesite and other alteration products are deformed as the slabs descend into the mantle. Low pressure experiments that were performed on magnesite indicate that it will be weaker than olivine in subducting slabs. However, these experiments did not determine the effects of grain size on the strength of magnesite by any high pressure deformation mechanisms. We deformed stacked cylinders of coarse (100µm) and fine-grain (1µm) magnesite in order to test how grain size affects the strength of magnesite deforming by dislocation glide and twinning at low temperatures.

A magnesite stack was deformed at T = 500oC and strain rate of ~10-5/s at three sequential pressures (~2, 3.5, 5 GPa). At each condition, the coarse-grained magnesite was weaker than the fine-grained magnesite. This result is consistent with previous experiments performed on calcite aggregates of different grain sizes, which showed grain boundary hardening by Hall-Petch mechanisms in the absence of recovery mechanisms. This result predicts that coarse-grain magnesite in subducting slabs will be weaker than fine-grain magnesite aggregates and strain localization where grain growth leads to coarse grain size.

Geological Society of America Abstracts with Programs. Vol. 49, No. 2

doi: 10.1130/abs/2017NE-290651

© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.