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History of the Development of Constitutive Equations for Strain-Rate-Metry from Microstructures


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1 Department of Geology, Jogamaya Devi College, Kolkata 700 026, India
     

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The measurement of strain rate (strain-rate-metry) from microstructures started in early 1970s. Earlier the strain rate was measured from the constitutive equations for stress-temperature-strain rate relations formulated from laboratory experiments. Later the term of water fugacity was included in these constitutive equations. In the late 1990s, a new model was formulated to measure strain rate from the shape of the recrystallized quartz grains, by measuring their area-perimeter fractal dimensions. This review describes the history of development of the different models of strain-ratemetry over the last five decades.

Keywords

Strain Rate, Flow Laws, Grain Diameter, Area-perimeter Fractal Dimension, Dynamic Recrystallization, Microstructures, Shear Zone.
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  • History of the Development of Constitutive Equations for Strain-Rate-Metry from Microstructures

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Authors

Bhaskar Ghosh
Department of Geology, Jogamaya Devi College, Kolkata 700 026, India

Abstract


The measurement of strain rate (strain-rate-metry) from microstructures started in early 1970s. Earlier the strain rate was measured from the constitutive equations for stress-temperature-strain rate relations formulated from laboratory experiments. Later the term of water fugacity was included in these constitutive equations. In the late 1990s, a new model was formulated to measure strain rate from the shape of the recrystallized quartz grains, by measuring their area-perimeter fractal dimensions. This review describes the history of development of the different models of strain-ratemetry over the last five decades.

Keywords


Strain Rate, Flow Laws, Grain Diameter, Area-perimeter Fractal Dimension, Dynamic Recrystallization, Microstructures, Shear Zone.

References





DOI: https://doi.org/10.24906/isc%2F2020%2Fv34%2Fi6%2F208221