From 14680273bf5d3dbc135e5246c12e51299deb6ac4 Mon Sep 17 00:00:00 2001 From: dansand Date: Thu, 29 Feb 2024 10:35:14 +1100 Subject: [PATCH 1/2] add a doi fiel to the YAML, and a metadata --- .../models/corcho-2022-collision/index.md | 1 + .../models/mather-2022-groundwater/index.md | 1 + src/pages/models/polanco-2023-deltas/index.md | 1 + .../models/sandiford-2021-detachment/index.md | 1 + .../models/sandiford-2024-detachment/index.md | 127 ++++++++++++++++++ src/templates/model.js | 34 ++++- 6 files changed, 164 insertions(+), 1 deletion(-) create mode 100644 src/pages/models/sandiford-2024-detachment/index.md diff --git a/src/pages/models/corcho-2022-collision/index.md b/src/pages/models/corcho-2022-collision/index.md index 49b2b03..ca21d0c 100644 --- a/src/pages/models/corcho-2022-collision/index.md +++ b/src/pages/models/corcho-2022-collision/index.md @@ -8,6 +8,7 @@ for_codes: - 3706 - 370604 status: completed +doi: software: - name: UWGeodynamics doi: 10.5281/zenodo.5606117 diff --git a/src/pages/models/mather-2022-groundwater/index.md b/src/pages/models/mather-2022-groundwater/index.md index d2dc4e8..03ba35f 100644 --- a/src/pages/models/mather-2022-groundwater/index.md +++ b/src/pages/models/mather-2022-groundwater/index.md @@ -11,6 +11,7 @@ for_codes: - 040601 - 040301 status: completed +doi: software: - name: Underworld2 doi: 10.5281/zenodo.7455999 diff --git a/src/pages/models/polanco-2023-deltas/index.md b/src/pages/models/polanco-2023-deltas/index.md index 199334b..4adc07a 100644 --- a/src/pages/models/polanco-2023-deltas/index.md +++ b/src/pages/models/polanco-2023-deltas/index.md @@ -10,6 +10,7 @@ for_codes: - 0406 - 040601 status: completed +doi: 10.5194/egusphere-2023-53 software: - name: Badlands doi: 10.5281/zenodo.1069573 diff --git a/src/pages/models/sandiford-2021-detachment/index.md b/src/pages/models/sandiford-2021-detachment/index.md index 751d640..e8f2d5d 100644 --- a/src/pages/models/sandiford-2021-detachment/index.md +++ b/src/pages/models/sandiford-2021-detachment/index.md @@ -8,6 +8,7 @@ for_codes: - 3706 - 370604 status: completed +doi: "" software: - name: ASPECT doi: 10.5281/zenodo.6903424 diff --git a/src/pages/models/sandiford-2024-detachment/index.md b/src/pages/models/sandiford-2024-detachment/index.md new file mode 100644 index 0000000..658df4a --- /dev/null +++ b/src/pages/models/sandiford-2024-detachment/index.md @@ -0,0 +1,127 @@ +--- +templateKey: model +slug: sandiford_2024_detachment +title: 'Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid‐Block + Rotation and Apparent Unbending' +date: '2024-02-22T23:03:42.000Z' +featuredpost: +doi: +for_codes: + - 2020 + - 370401 +status: +software: + - name: 'geodynamics/aspect: ASPECT 2.5.0' + doi: https://doi.org/10.5281/zenodo.8200213 + url_source: +licence: + licence_url: https://creativecommons.org/licenses/by/4.0/legalcode + licence_image: ../../../img/licence/by.png + description: Creative Commons Attribution 4.0 International + licence_file: +contributor: + name: Dan + family_name: Sandiford + ORCID: https://orcid.org/0000-0002-2207-6837 +authors: + - name: Dan + family_name: Sandiford + ORCID: 0000-0002-2207-6837 + - name: Sascha + family_name: Brune + ORCID: http://orcid.org/0000-0003-4985-1810 + - name: Anne + family_name: Glerum + ORCID: http://orcid.org/0000-0002-9481-1749 + - name: John + family_name: Naliboff + ORCID: http://orcid.org/0000-0002-5697-7203 + - name: Joanne M. + family_name: Whittaker + ORCID: http://orcid.org/0000-0002-3170-3935 +associated_publication: + title: 'Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid‐Block + Rotation and Apparent Unbending' + journal: Geochemistry, Geophysics, Geosystems + publisher: American Geophysical Union (AGU) + doi: http://dx.doi.org/10.1029/2021gc009681 + url: +compute_info: + name: + organisation: + computer_url: https://dx.doi.org/10.25914/608bfd1838db2 + computer_doi: +research_tags: + - +compute_tags: + - C++ + - finite-element + - mesh-refinement +grants_funder: + doi: + number_id: + url: +abstract: Seafloor spreading at slow rates can be accommodated on large‐offset oceanic + detachment faults (ODFs), that exhume lower crustal and mantle rocks in footwall + domes termed oceanic core complexes (OCCs). Footwall rocks experience large rotation + during exhumation, yet important aspects of the kinematics—particularly the relative + roles of solid‐block rotation and flexure—are not clearly understood. Using a high‐resolution + numerical model, we explore the exhumation kinematics in the footwall beneath an + emergent ODF/OCC. A key feature of the models is that footwall motion is dominated + by solid‐block rotation, accommodated by the nonplanar, concave‐down fault interface. + A consequence is that curvature measured along the ODF is representative of a neutral + stress configuration, rather than a “bent” one. Instead, it is in the subsequent + process of “apparent unbending” that significant flexural stresses are developed + in the model footwall. The brittle strain associated with apparent unbending is + produced dominantly in extension, beneath the OCC, consistent with earthquake clustering + observed in the Trans‐Atlantic Geotraverse at the Mid‐Atlantic Ridge. +images: + landing_image: + src: ./graphics/fig1.png + caption: Deviatoric stresses and vorticity in reference model. + graphic_abstract: + src: ./graphics/fig4.png + caption: fig4.png + model_setup: + src: + caption: +animation: + src: animation.mp4 + caption: Animation for alternative model showing vorticity. +model_setup_info: + url: + summary: The domain is $400 \; \mathrm{km}$ wide and $100 \; \mathrm{km}$ deep, + and includes five levels of mesh refinement, as shown in the figure. The model + is initialised with a symmetric temperature structure, defined by a transient + 1-D cooling profile, with an age of $0.5 \; \mathrm{Myr}$ in the center of the + domain. The thermal profile ages outwardly in proportion to the applied spreading + rate of $2 \; \mathrm{cm\,{yr}^{-1}}$ (full rate), which is representative for + slow spreading ridges. Uniform inflow at the bottom boundary balances the outward + flux of material at the side boundaries. The model has a true free surface, and + a diffusion process is applied to the surface topography in order to counteract + strong mesh deformation. A simplification here is that the effect of the water + column is ignored, i.e. the detachment system is modeled as sub-aerial. There + is no compositional differentiation in the model (i.e. no crust/mantle) and all + parts of the domain are subject to the same constitutive model. The constitutive + model incorporates viscous (dislocation creep), elastic and plastic (pseudo-brittle) + deformation mechanisms, hereafter referred to as visco-elastic plastic (VEP) rheology, + following the approach of Moresi et al. (2003). The advection-diffusion equation + included an anomalously- high diffusivity $(3 \times {10}^{-6} \; \mathrm{m^2 + \, s^{-1}})$ which is intended to model the near axis cooling effect of hydrothermal + circulation (cf. Lavier and Buck, 2002). As implemented here, the higher diffusivity + applies throughout the domain, rather than being localized at the ridge (as in + Lavier and Buck, 2002). The parameters chosen here result in $\sim 10 \; \mathrm{km}$ + lithosphere at the ridge axis, which is in the range identified for ODF development. + Due to the difference in diffusivity values in the initial conditions $({10}^{-6} + \; \mathrm{m^2 \, s^{-1}})$, and temperature evolution equation $(3 \times {10}^{-6})$, + the thermal structure is not in steady state and some cooling of the off-axis + lithosphere occurs. +model_files: + url: + notes: + file_tree: +dataset: + url: + notes: + doi: +--- diff --git a/src/templates/model.js b/src/templates/model.js index c104696..2c1c4f0 100644 --- a/src/templates/model.js +++ b/src/templates/model.js @@ -43,6 +43,7 @@ const ModelTemplate = ({ research_tags, title, slug, + doi, }) => { const PostContent = contentComponent || Content const dataset_url = ( @@ -132,10 +133,12 @@ const ModelTemplate = ({
-

Abstract

+

Description

{abstract}

+ + { publication &&
@@ -175,6 +178,33 @@ const ModelTemplate = ({
} + + { + doi && +
+

Metadata & citation

+ { + doi && + + } + + { + licence_content && + +
{licence_content}
+ + } +
+ } + + +

Licence

@@ -388,6 +418,7 @@ const ModelsPage = ({ data }) => { research_tags={post.frontmatter.research_tags} title={post.frontmatter.title} slug={post.frontmatter.slug} + doi={post.frontmatter.doi} /> ) @@ -406,6 +437,7 @@ export const pageQuery = graphql` frontmatter { abstract slug + doi animations { caption src { From 4a69ad9d1b0821c4c3ee3a804341e651f01a1cf8 Mon Sep 17 00:00:00 2001 From: dansand Date: Fri, 1 Mar 2024 12:04:20 +1100 Subject: [PATCH 2/2] remove dummy model --- .../models/sandiford-2024-detachment/index.md | 127 ------------------ 1 file changed, 127 deletions(-) delete mode 100644 src/pages/models/sandiford-2024-detachment/index.md diff --git a/src/pages/models/sandiford-2024-detachment/index.md b/src/pages/models/sandiford-2024-detachment/index.md deleted file mode 100644 index 658df4a..0000000 --- a/src/pages/models/sandiford-2024-detachment/index.md +++ /dev/null @@ -1,127 +0,0 @@ ---- -templateKey: model -slug: sandiford_2024_detachment -title: 'Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid‐Block - Rotation and Apparent Unbending' -date: '2024-02-22T23:03:42.000Z' -featuredpost: -doi: -for_codes: - - 2020 - - 370401 -status: -software: - - name: 'geodynamics/aspect: ASPECT 2.5.0' - doi: https://doi.org/10.5281/zenodo.8200213 - url_source: -licence: - licence_url: https://creativecommons.org/licenses/by/4.0/legalcode - licence_image: ../../../img/licence/by.png - description: Creative Commons Attribution 4.0 International - licence_file: -contributor: - name: Dan - family_name: Sandiford - ORCID: https://orcid.org/0000-0002-2207-6837 -authors: - - name: Dan - family_name: Sandiford - ORCID: 0000-0002-2207-6837 - - name: Sascha - family_name: Brune - ORCID: http://orcid.org/0000-0003-4985-1810 - - name: Anne - family_name: Glerum - ORCID: http://orcid.org/0000-0002-9481-1749 - - name: John - family_name: Naliboff - ORCID: http://orcid.org/0000-0002-5697-7203 - - name: Joanne M. - family_name: Whittaker - ORCID: http://orcid.org/0000-0002-3170-3935 -associated_publication: - title: 'Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid‐Block - Rotation and Apparent Unbending' - journal: Geochemistry, Geophysics, Geosystems - publisher: American Geophysical Union (AGU) - doi: http://dx.doi.org/10.1029/2021gc009681 - url: -compute_info: - name: - organisation: - computer_url: https://dx.doi.org/10.25914/608bfd1838db2 - computer_doi: -research_tags: - - -compute_tags: - - C++ - - finite-element - - mesh-refinement -grants_funder: - doi: - number_id: - url: -abstract: Seafloor spreading at slow rates can be accommodated on large‐offset oceanic - detachment faults (ODFs), that exhume lower crustal and mantle rocks in footwall - domes termed oceanic core complexes (OCCs). Footwall rocks experience large rotation - during exhumation, yet important aspects of the kinematics—particularly the relative - roles of solid‐block rotation and flexure—are not clearly understood. Using a high‐resolution - numerical model, we explore the exhumation kinematics in the footwall beneath an - emergent ODF/OCC. A key feature of the models is that footwall motion is dominated - by solid‐block rotation, accommodated by the nonplanar, concave‐down fault interface. - A consequence is that curvature measured along the ODF is representative of a neutral - stress configuration, rather than a “bent” one. Instead, it is in the subsequent - process of “apparent unbending” that significant flexural stresses are developed - in the model footwall. The brittle strain associated with apparent unbending is - produced dominantly in extension, beneath the OCC, consistent with earthquake clustering - observed in the Trans‐Atlantic Geotraverse at the Mid‐Atlantic Ridge. -images: - landing_image: - src: ./graphics/fig1.png - caption: Deviatoric stresses and vorticity in reference model. - graphic_abstract: - src: ./graphics/fig4.png - caption: fig4.png - model_setup: - src: - caption: -animation: - src: animation.mp4 - caption: Animation for alternative model showing vorticity. -model_setup_info: - url: - summary: The domain is $400 \; \mathrm{km}$ wide and $100 \; \mathrm{km}$ deep, - and includes five levels of mesh refinement, as shown in the figure. The model - is initialised with a symmetric temperature structure, defined by a transient - 1-D cooling profile, with an age of $0.5 \; \mathrm{Myr}$ in the center of the - domain. The thermal profile ages outwardly in proportion to the applied spreading - rate of $2 \; \mathrm{cm\,{yr}^{-1}}$ (full rate), which is representative for - slow spreading ridges. Uniform inflow at the bottom boundary balances the outward - flux of material at the side boundaries. The model has a true free surface, and - a diffusion process is applied to the surface topography in order to counteract - strong mesh deformation. A simplification here is that the effect of the water - column is ignored, i.e. the detachment system is modeled as sub-aerial. There - is no compositional differentiation in the model (i.e. no crust/mantle) and all - parts of the domain are subject to the same constitutive model. The constitutive - model incorporates viscous (dislocation creep), elastic and plastic (pseudo-brittle) - deformation mechanisms, hereafter referred to as visco-elastic plastic (VEP) rheology, - following the approach of Moresi et al. (2003). The advection-diffusion equation - included an anomalously- high diffusivity $(3 \times {10}^{-6} \; \mathrm{m^2 - \, s^{-1}})$ which is intended to model the near axis cooling effect of hydrothermal - circulation (cf. Lavier and Buck, 2002). As implemented here, the higher diffusivity - applies throughout the domain, rather than being localized at the ridge (as in - Lavier and Buck, 2002). The parameters chosen here result in $\sim 10 \; \mathrm{km}$ - lithosphere at the ridge axis, which is in the range identified for ODF development. - Due to the difference in diffusivity values in the initial conditions $({10}^{-6} - \; \mathrm{m^2 \, s^{-1}})$, and temperature evolution equation $(3 \times {10}^{-6})$, - the thermal structure is not in steady state and some cooling of the off-axis - lithosphere occurs. -model_files: - url: - notes: - file_tree: -dataset: - url: - notes: - doi: ----