File:Layered Websterite in Basement Sill in McMurdo Dry Valleys in Antarctica.jpg
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English: Layered websterite in Basement Sill in McMurdo Dry Valleys in Antarctica.
Small scale, rhythmic layering in the LZ websterite comprising thin bands of plagioclase dispersed within a predominantly Opx matrix. Model-derived shear strain rates for congested magma where crystal loads exceed approximately 30% are comparable with experimental evidence for shear-thinning in congested magmas. The implication is that the feldspar-rich layers formed by dilation in the magma slurry during emplacement. |
| Date | (publication date of source article) |
| Source | Figure 17 in Petford, N. and Mirhadizadeh S. (2017) Image-based modelling of lateral magma flow: the Basement Sill, Antarctica, Royal Society Open Science, Volume 4, Issue 5, May 2017, DOI: 10.1098/rsos.161083 http://rsos.royalsocietypublishing.org/content/4/5/161083 |
| Author | Nick Petford and Seyed Mirhadizadeh |
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Figure 17 in Petford, N. and Mirhadizadeh S. (2017) Image-based modelling of lateral magma flow: the Basement Sill, Antarctica, Royal Society Open Science, Volume 4, Issue 5, May 2017, DOI: 10.1098/rsos.161083 http://rsos.royalsocietypublishing.org/content/4/5/161083, was reviewed on 27 May 2018 by reviewer Leoboudv, who confirmed that it was available there under the stated license on that date.
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| current | 18:09, 26 May 2018 | | 1,280 × 961 (259 KB) | GeoWriter (talk | contribs) | User created page with UploadWizard |
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