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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Bibliographic Details
Main Authors: Petford, Nick, Mirhadizadeh, Seyed
Format: Dataset
Language:English
Published: Dryad 2017
Subjects:
Online Access:https://dx.doi.org/10.5061/dryad.sn69s
https://datadryad.org/stash/dataset/doi:10.5061/dryad.sn69s
id ftdatacite:10.5061/dryad.sn69s
record_format openpolar
spelling 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
institution 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
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