Data from: Image based modelling of lateral magma flow: the Basement Sill, Antarctica ...
The McMurdo Dry Valleys magmatic system, Antarctica, provides a world-class example of pervasive lateral magma flow on a continental scale. The lowermost intrusion (Basement Sill) offers detailed sections through the now frozen particle microstructure of a congested magma slurry. We simulated the fl...
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Online Access: | https://dx.doi.org/10.5061/dryad.sn69s https://datadryad.org/stash/dataset/doi:10.5061/dryad.sn69s |
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ftdatacite:10.5061/dryad.sn69s 2024-06-09T07:39:05+00:00 Data from: Image based modelling of lateral magma flow: the Basement Sill, Antarctica ... Petford, Nick Mirhadizadeh, Seyed 2017 https://dx.doi.org/10.5061/dryad.sn69s https://datadryad.org/stash/dataset/doi:10.5061/dryad.sn69s en eng Dryad https://dx.doi.org/10.1098/rsos.161083 Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 Sill Rheology Igneous intrusion Dataset dataset 2017 ftdatacite https://doi.org/10.5061/dryad.sn69s10.1098/rsos.161083 2024-05-13T10:59:08Z The McMurdo Dry Valleys magmatic system, Antarctica, provides a world-class example of pervasive lateral magma flow on a continental scale. The lowermost intrusion (Basement Sill) offers detailed sections through the now frozen particle microstructure of a congested magma slurry. We simulated the flow regime in two and three dimensions using numerical models built on a finite-element mesh derived from field data. The model captures the flow behaviour of the Basement Sill magma over a viscosity range of 1–104 Pa s where the higher end (greater than or equal to 102 Pa s) corresponds to a magmatic slurry with crystal fractions varying between 30 and 70%. A novel feature of the model is the discovery of transient, low viscosity (less than or equal to 50 Pa s) high Reynolds number eddies formed along undulating contacts at the floor and roof of the intrusion. Numerical tracing of particle orbits implies crystals trapped in eddies segregate according to their mass density. Recovered shear strain rates (10−3–10−5 ... : Supplementary MaterialsAdditional data on model runs. This folder contains supplementary figures in ppt and video clips of model test runs and of particle circulation paths. Data include 2 and 3D visualisations, calculations of shear rate and Reynolds numbers and other parameters arising from the model simulations.Supplementary_Materials.zip ... Dataset Antarc* Antarctica McMurdo Dry Valleys DataCite Metadata Store (German National Library of Science and Technology) McMurdo Dry Valleys |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Sill Rheology Igneous intrusion |
spellingShingle |
Sill Rheology Igneous intrusion Petford, Nick Mirhadizadeh, Seyed Data from: Image based modelling of lateral magma flow: the Basement Sill, Antarctica ... |
topic_facet |
Sill Rheology Igneous intrusion |
description |
The McMurdo Dry Valleys magmatic system, Antarctica, provides a world-class example of pervasive lateral magma flow on a continental scale. The lowermost intrusion (Basement Sill) offers detailed sections through the now frozen particle microstructure of a congested magma slurry. We simulated the flow regime in two and three dimensions using numerical models built on a finite-element mesh derived from field data. The model captures the flow behaviour of the Basement Sill magma over a viscosity range of 1–104 Pa s where the higher end (greater than or equal to 102 Pa s) corresponds to a magmatic slurry with crystal fractions varying between 30 and 70%. A novel feature of the model is the discovery of transient, low viscosity (less than or equal to 50 Pa s) high Reynolds number eddies formed along undulating contacts at the floor and roof of the intrusion. Numerical tracing of particle orbits implies crystals trapped in eddies segregate according to their mass density. Recovered shear strain rates (10−3–10−5 ... : Supplementary MaterialsAdditional data on model runs. This folder contains supplementary figures in ppt and video clips of model test runs and of particle circulation paths. Data include 2 and 3D visualisations, calculations of shear rate and Reynolds numbers and other parameters arising from the model simulations.Supplementary_Materials.zip ... |
format |
Dataset |
author |
Petford, Nick Mirhadizadeh, Seyed |
author_facet |
Petford, Nick Mirhadizadeh, Seyed |
author_sort |
Petford, Nick |
title |
Data from: Image based modelling of lateral magma flow: the Basement Sill, Antarctica ... |
title_short |
Data from: Image based modelling of lateral magma flow: the Basement Sill, Antarctica ... |
title_full |
Data from: Image based modelling of lateral magma flow: the Basement Sill, Antarctica ... |
title_fullStr |
Data from: Image based modelling of lateral magma flow: the Basement Sill, Antarctica ... |
title_full_unstemmed |
Data from: Image based modelling of lateral magma flow: the Basement Sill, Antarctica ... |
title_sort |
data from: image based modelling of lateral magma flow: the basement sill, antarctica ... |
publisher |
Dryad |
publishDate |
2017 |
url |
https://dx.doi.org/10.5061/dryad.sn69s https://datadryad.org/stash/dataset/doi:10.5061/dryad.sn69s |
geographic |
McMurdo Dry Valleys |
geographic_facet |
McMurdo Dry Valleys |
genre |
Antarc* Antarctica McMurdo Dry Valleys |
genre_facet |
Antarc* Antarctica McMurdo Dry Valleys |
op_relation |
https://dx.doi.org/10.1098/rsos.161083 |
op_rights |
Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 |
op_doi |
https://doi.org/10.5061/dryad.sn69s10.1098/rsos.161083 |
_version_ |
1801377097541746688 |