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- Q18670390 subject Q7037486.
- Q18670390 abstract "Strain partitioning is commonly referred to as a deformation process in which the total strain experienced on a rock, area, or region, is heterogeneously distributed in terms of the strain intensity and strain type (i.e. pure shear, simple shear, dilatation). This process is observed on a range of scales spanning from the grain – crystal scale to the plate – lithospheric scale, and occurs in both the brittle and plastic deformation regimes. The manner and intensity by which strain is distributed are controlled by a number of factors listed below.".
- Q18670390 wikiPageWikiLink Q1255282.
- Q18670390 wikiPageWikiLink Q15300737.
- Q18670390 wikiPageWikiLink Q1578160.
- Q18670390 wikiPageWikiLink Q176318.
- Q18670390 wikiPageWikiLink Q193514.
- Q18670390 wikiPageWikiLink Q1963861.
- Q18670390 wikiPageWikiLink Q2672013.
- Q18670390 wikiPageWikiLink Q271707.
- Q18670390 wikiPageWikiLink Q43533.
- Q18670390 wikiPageWikiLink Q4462148.
- Q18670390 wikiPageWikiLink Q44626.
- Q18670390 wikiPageWikiLink Q466686.
- Q18670390 wikiPageWikiLink Q47089.
- Q18670390 wikiPageWikiLink Q496325.
- Q18670390 wikiPageWikiLink Q5156153.
- Q18670390 wikiPageWikiLink Q5251699.
- Q18670390 wikiPageWikiLink Q5451.
- Q18670390 wikiPageWikiLink Q7037486.
- Q18670390 wikiPageWikiLink Q7320412.
- Q18670390 wikiPageWikiLink Q7520832.
- Q18670390 wikiPageWikiLink Q7623760.
- Q18670390 wikiPageWikiLink Q7835340.
- Q18670390 wikiPageWikiLink Q7950.
- Q18670390 wikiPageWikiLink Q920070.
- Q18670390 comment "Strain partitioning is commonly referred to as a deformation process in which the total strain experienced on a rock, area, or region, is heterogeneously distributed in terms of the strain intensity and strain type (i.e. pure shear, simple shear, dilatation). This process is observed on a range of scales spanning from the grain – crystal scale to the plate – lithospheric scale, and occurs in both the brittle and plastic deformation regimes.".
- Q18670390 label "Strain partitioning".