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Model category Warning: No category selected Scientific keywords Warning: No keywords given Include model code? Error: no selection made Model code URI/DOI Warning: No URI/DOI provided. Include model output data? Error: no selection made Model output URI/DOI Warning: No URI/DOI provided. Software Framework DOI/URI Warning: no DOI/URI provided. Software Repository Warning: no repository URL provided. Name of primary software framework Error: no name found Software framework authors Error: no authors found Software & algorithm keywords Warning: no keywords given. Computer URI/DOI Warning: No URI/DOI provided. Landing page image Error: No image uploaded.

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Parsed data

Section 1: Summary of your model

Creator/Contributor Creator/contributor is Dan Sandiford (0000-0002-2207-6837)

Model Repository Slug Model repo will be created with name foo_1972_model

Field of Research (FoR) Codes

#FoR_370604: Geodynamics

License GNU Affero General Public License v3.0

Model Category

Associated Publication Found publication: Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid‐Block Rotation and Apparent Unbending

Title Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid‐Block Rotation and Apparent Unbending

Description 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.

Model Authors

Dan Sandiford (0000-0002-2207-6837)
Sascha Brune (0000-0003-4985-1810)
Anne Glerum (0000-0002-9481-1749)
John Naliboff (0000-0002-5697-7203)
Joanne M. Whittaker (0000-0002-3170-3935)

Funder

Helmholtz Association

Section 2: your model code, output data

Section 3: software framework and compute details

Section 4: web material (for mate.science)

Dumping dictionary during testing {'creator': {'@type': 'Person', '@id': 'https://orcid.org/0000-0002-2207-6837', 'givenName': 'Dan', 'familyName': 'Sandiford'}, 'slug': 'foo_1972_model', 'for_codes': [{'@id': '#FoR_370604', '@type': 'DefinedTerm', 'name': 'Geodynamics'}], 'license': {'name': 'GNU Affero General Public License v3.0', 'url': 'https://www.gnu.org/licenses/agpl-3.0.txt'}, 'model_category': [], 'publication': {'@type': 'ScholarlyArticle', '@id': 'http://dx.doi.org/10.1029/2021gc009681', 'name': 'Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid‐Block Rotation and Apparent Unbending', 'isPartOf': ({'@type': 'PublicationIssue', 'issueNumber': '4', 'datePublished': '2021-4', 'isPartOf': {'@type': ['PublicationVolume', 'Periodical'], 'name': ['Geochemistry, Geophysics, Geosystems'], 'issn': ['1525-2027', '1525-2027'], 'volumeNumber': '22', 'publisher': 'American Geophysical Union (AGU)'}},), 'author': [{'@type': 'Person', '@id': 'http://orcid.org/0000-0002-2207-6837', 'givenName': 'Dan', 'familyName': 'Sandiford', 'affiliation': [{'@type': 'Organization', 'name': 'Institute for Marine and Antarctic Studies University of Tasmania Hobart TAS Australia'}, {'@type': 'Organization', 'name': 'Helmholtz Centre Potsdam—German Research Centre for Geosciences (GFZ) Potsdam Germany'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0003-4985-1810', 'givenName': 'Sascha', 'familyName': 'Brune', 'affiliation': [{'@type': 'Organization', 'name': 'Helmholtz Centre Potsdam—German Research Centre for Geosciences (GFZ) Potsdam Germany'}, {'@type': 'Organization', 'name': 'Institute of Geosciences University of Potsdam Potsdam Germany'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-9481-1749', 'givenName': 'Anne', 'familyName': 'Glerum', 'affiliation': [{'@type': 'Organization', 'name': 'Helmholtz Centre Potsdam—German Research Centre for Geosciences (GFZ) Potsdam Germany'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-5697-7203', 'givenName': 'John', 'familyName': 'Naliboff', 'affiliation': [{'@type': 'Organization', 'name': 'Department of Earth and Environmental Science New Mexico Institute of Mining and Technology Socorro NM USA'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-3170-3935', 'givenName': 'Joanne M.', 'familyName': 'Whittaker', 'affiliation': [{'@type': 'Organization', 'name': 'Institute for Marine and Antarctic Studies University of Tasmania Hobart TAS Australia'}]}], '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.', 'identifier': ['10.1029/2021GC009681'], 'funder': [{'@type': 'Organization', 'name': 'Helmholtz Association'}]}, 'title': 'Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid‐Block Rotation and Apparent Unbending', 'description': '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.', 'authors': [{'@type': 'Person', '@id': 'http://orcid.org/0000-0002-2207-6837', 'givenName': 'Dan', 'familyName': 'Sandiford', 'affiliation': [{'@type': 'Organization', 'name': 'Institute for Marine and Antarctic Studies University of Tasmania Hobart TAS Australia'}, {'@type': 'Organization', 'name': 'Helmholtz Centre Potsdam—German Research Centre for Geosciences (GFZ) Potsdam Germany'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0003-4985-1810', 'givenName': 'Sascha', 'familyName': 'Brune', 'affiliation': [{'@type': 'Organization', 'name': 'Helmholtz Centre Potsdam—German Research Centre for Geosciences (GFZ) Potsdam Germany'}, {'@type': 'Organization', 'name': 'Institute of Geosciences University of Potsdam Potsdam Germany'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-9481-1749', 'givenName': 'Anne', 'familyName': 'Glerum', 'affiliation': [{'@type': 'Organization', 'name': 'Helmholtz Centre Potsdam—German Research Centre for Geosciences (GFZ) Potsdam Germany'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-5697-7203', 'givenName': 'John', 'familyName': 'Naliboff', 'affiliation': [{'@type': 'Organization', 'name': 'Department of Earth and Environmental Science New Mexico Institute of Mining and Technology Socorro NM USA'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-3170-3935', 'givenName': 'Joanne M.', 'familyName': 'Whittaker', 'affiliation': [{'@type': 'Organization', 'name': 'Institute for Marine and Antarctic Studies University of Tasmania Hobart TAS Australia'}]}], 'keywords': [], 'funder': [{'@type': 'Organization', 'name': 'Helmholtz Association'}], 'software': {'@type': 'SoftwareApplication'}}

hvidy / PIPE-4002-EarthByte-ModelAtlas

M@TE submission request from @dansand #28

-> creator/contributor ORCID (or name)

-> slug

-> field of Research (FoR) Codes

-> license

-> model category

-> associated publication DOI

-> title

-> description

-> model authors

-> scientific keywords

-> funder

-> include model code ?

-> model code URI/DOI

-> include model output data?

-> model output URI/DOI

-> software framework DOI/URI

-> software framework source repository

-> name of primary software framework (e.g. Underworld, ASPECT, Badlands, OpenFOAM)

-> software framework authors

-> software & algorithm keywords

-> computer URI/DOI

-> add landing page image and caption

-> add an animation (if relevant)

-> add a graphic abstract figure (if relevant)

-> add a model setup figure (if relevant)