Shear stress along active megathrusts and force balance solutions
The data are the source data for Figures 2, 3, and 4 in the paper "Megathrust shear force controls mountain height at convergent plate margins" by Dielforder, Hetzel, and Oncken (2020). Details on the calculation of the data are given in the methods section of this paper. The archive "...
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GFZ Data Services
2020
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Online Access: | https://dx.doi.org/10.5880/gfz.4.1.2020.002 https://dataservices.gfz-potsdam.de/panmetaworks/showshort.php?id=escidoc:5034890 |
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Topography mountain height force balance EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > STRESS EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > PLATE BOUNDARIES EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS |
spellingShingle |
Topography mountain height force balance EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > STRESS EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > PLATE BOUNDARIES EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS Dielforder, Armin Hetzel, Ralf Oncken, Onno Shear stress along active megathrusts and force balance solutions |
topic_facet |
Topography mountain height force balance EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > STRESS EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > PLATE BOUNDARIES EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS |
description |
The data are the source data for Figures 2, 3, and 4 in the paper "Megathrust shear force controls mountain height at convergent plate margins" by Dielforder, Hetzel, and Oncken (2020). Details on the calculation of the data are given in the methods section of this paper. The archive "2020-002_Dielforder-et-al_shear_stress_envelopes.zip" includes ten csv-files entitled "n_shear_stress_envelope.csv", where n is a number from 1 to 10 and refers to the margin transects studied in the paper (for labeling see below). The files provide the source data for the ten shear stress envelopes shown in Figure 2. In each file, the values in the first, second, and third column are depth (m), shear stress (MPa), and the one standard deviation of the shear stress (MPa), respectively. The archive "2020-002_Dielforder-et-al_shear_force_solutions.zip" contains one csv-file including 100,000 model solutions for the megathrust shear force (TN m-1). Columns 1 to 10 contain the solutions for the respective margin transects. The archive "2020-002_Dielforder-et-al_force_balance_solutions.zip" includes ten csv-files entitled "n_force_balance_solutions.csv" following the same labeling scheme as above. The values in the first, second, and third column are the 100,000 model solutions for the tectonically supported elevation TSE (m), the shear-force component required to support the submarine margin topography F_SMT (TN m-1), and the shear-force component available to support subaerial mountain height [delta]F_s (TN m-1), respectively. For the Himalayas (10_force_balance_solutions.csv), there are only values in the first column, because the Himalayas have no submarine margin topography. The 100,000 model solutions were used to calculate the mean values and one standard deviation shown in Figures 3 and 4 and listed in Table 1 and Extended Data Table 3. Labeling: 1, Northern Cascadia; 2, 3, and 4, Andes at 23º S, 34º S, and 36º S, respectively; 5, Northern Sumatra; 6, Kamchatka; 7, Japan Trench; 8, Nankai Trough; 9, Northern Hikurangi; 10, Himalayas. The references listed below provide the input parameters used to calculate the shear stress envelopes, F_s, TSE, F_SMT and [delta]Fs. |
format |
Dataset |
author |
Dielforder, Armin Hetzel, Ralf Oncken, Onno |
author_facet |
Dielforder, Armin Hetzel, Ralf Oncken, Onno |
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Dielforder, Armin |
title |
Shear stress along active megathrusts and force balance solutions |
title_short |
Shear stress along active megathrusts and force balance solutions |
title_full |
Shear stress along active megathrusts and force balance solutions |
title_fullStr |
Shear stress along active megathrusts and force balance solutions |
title_full_unstemmed |
Shear stress along active megathrusts and force balance solutions |
title_sort |
shear stress along active megathrusts and force balance solutions |
publisher |
GFZ Data Services |
publishDate |
2020 |
url |
https://dx.doi.org/10.5880/gfz.4.1.2020.002 https://dataservices.gfz-potsdam.de/panmetaworks/showshort.php?id=escidoc:5034890 |
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Kamchatka |
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CC BY 4.0 http://creativecommons.org/licenses/by/4.0 |
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https://doi.org/10.5880/gfz.4.1.2020.002 https://doi.org/doi of paper when available https://doi.org/10.7289/v5c8276m https://doi.org/10.1038/417536a https://doi.org/10.1016/j.epsl.2017.06.021 https://doi.org/10.1029/2005jb003916 https://doi.o |
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ftdatacite:10.5880/gfz.4.1.2020.002 2023-05-15T16:59:31+02:00 Shear stress along active megathrusts and force balance solutions Dielforder, Armin Hetzel, Ralf Oncken, Onno 2020 application/octet-stream https://dx.doi.org/10.5880/gfz.4.1.2020.002 https://dataservices.gfz-potsdam.de/panmetaworks/showshort.php?id=escidoc:5034890 en eng GFZ Data Services https://dx.doi.org/doi of paper when available https://dx.doi.org/10.7289/v5c8276m https://dx.doi.org/10.1038/417536a https://dx.doi.org/10.1016/j.epsl.2017.06.021 https://dx.doi.org/10.1029/2005jb003916 https://dx.doi.org/10.1126/science.1255487 https://dx.doi.org/10.1029/2011jb008524 https://dx.doi.org/10.1126/science.aat4723 https://dx.doi.org/10.1029/2010gc003230 https://dx.doi.org/10.1029/2008jb005698 https://dx.doi.org/10.1016/j.tecto.2012.11.023 https://dx.doi.org/10.1029/2008jb005864 https://dx.doi.org/10.1029/2009jb006569 https://dx.doi.org/10.1126/science.1167719 https://dx.doi.org/10.1029/2002jb001771 https://dx.doi.org/10.1029/2005jb004108 https://dx.doi.org/10.1029/2012gl051308 https://dx.doi.org/10.1016/j.tecto.2012.07.009 https://dx.doi.org/10.1002/2014jb011170 https://dx.doi.org/10.1029/2003jb002958 https://dx.doi.org/10.1002/2017jb015384 https://dx.doi.org/10.1002/2015gl064845 https://dx.doi.org/10.1029/2005jb003976 https://dx.doi.org/10.1029/2009gc002610 https://dx.doi.org/10.1130/g30597.1 https://dx.doi.org/10.1029/1999jb900103 https://dx.doi.org/10.1785/0220130035 CC BY 4.0 http://creativecommons.org/licenses/by/4.0 CC-BY Topography mountain height force balance EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > STRESS EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > PLATE BOUNDARIES EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS dataset Dataset 2020 ftdatacite https://doi.org/10.5880/gfz.4.1.2020.002 https://doi.org/doi of paper when available https://doi.org/10.7289/v5c8276m https://doi.org/10.1038/417536a https://doi.org/10.1016/j.epsl.2017.06.021 https://doi.org/10.1029/2005jb003916 https://doi.o 2021-11-05T12:55:41Z The data are the source data for Figures 2, 3, and 4 in the paper "Megathrust shear force controls mountain height at convergent plate margins" by Dielforder, Hetzel, and Oncken (2020). Details on the calculation of the data are given in the methods section of this paper. The archive "2020-002_Dielforder-et-al_shear_stress_envelopes.zip" includes ten csv-files entitled "n_shear_stress_envelope.csv", where n is a number from 1 to 10 and refers to the margin transects studied in the paper (for labeling see below). The files provide the source data for the ten shear stress envelopes shown in Figure 2. In each file, the values in the first, second, and third column are depth (m), shear stress (MPa), and the one standard deviation of the shear stress (MPa), respectively. The archive "2020-002_Dielforder-et-al_shear_force_solutions.zip" contains one csv-file including 100,000 model solutions for the megathrust shear force (TN m-1). Columns 1 to 10 contain the solutions for the respective margin transects. The archive "2020-002_Dielforder-et-al_force_balance_solutions.zip" includes ten csv-files entitled "n_force_balance_solutions.csv" following the same labeling scheme as above. The values in the first, second, and third column are the 100,000 model solutions for the tectonically supported elevation TSE (m), the shear-force component required to support the submarine margin topography F_SMT (TN m-1), and the shear-force component available to support subaerial mountain height [delta]F_s (TN m-1), respectively. For the Himalayas (10_force_balance_solutions.csv), there are only values in the first column, because the Himalayas have no submarine margin topography. The 100,000 model solutions were used to calculate the mean values and one standard deviation shown in Figures 3 and 4 and listed in Table 1 and Extended Data Table 3. Labeling: 1, Northern Cascadia; 2, 3, and 4, Andes at 23º S, 34º S, and 36º S, respectively; 5, Northern Sumatra; 6, Kamchatka; 7, Japan Trench; 8, Nankai Trough; 9, Northern Hikurangi; 10, Himalayas. The references listed below provide the input parameters used to calculate the shear stress envelopes, F_s, TSE, F_SMT and [delta]Fs. Dataset Kamchatka DataCite Metadata Store (German National Library of Science and Technology) |