3-D thermal regime and petrologic metamorphism in Kuril-Kamchatka
The data include the 3-D temperature field (degrees Celsius), water content (wt%), dehydration rate (wt%/km), and subduction velocity field (cm/yr) of the subducting plate, as well as the coastline and volcano distribution in Kuril-Kamchatka. The data coordinates are an orthogonal coordinate system,...
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ftdans:oai:easy.dans.knaw.nl:easy-dataset:260627 2023-07-02T03:32:48+02:00 3-D thermal regime and petrologic metamorphism in Kuril-Kamchatka Ji, Y (via Mendeley Data) 2022-10-26T11:21:53.210Z http://nbn-resolving.org/urn:nbn:nl:ui:13-ym-ennn https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:260627 unknown 2 jgy68s9ttg http://nbn-resolving.org/urn:nbn:nl:ui:13-ym-ennn doi:10.17632/jgy68s9ttg.2 https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:260627 OPEN_ACCESS: The data are archived in Easy, they are accessible elsewhere through the DOI https://dans.knaw.nl/en/about/organisation-and-policy/legal-information/DANSLicence.pdf Yingfeng Ji Interdisciplinary sciences 2022 ftdans https://doi.org/10.17632/jgy68s9ttg.2 2023-06-13T12:55:01Z The data include the 3-D temperature field (degrees Celsius), water content (wt%), dehydration rate (wt%/km), and subduction velocity field (cm/yr) of the subducting plate, as well as the coastline and volcano distribution in Kuril-Kamchatka. The data coordinates are an orthogonal coordinate system, where the origin of the coordinates is (156.00E,47.18N), the x+ azimuth is 133 degrees clockwise from the north, and the y+ azimuth is 43 degrees clockwise from the north, and the z+ direction is vertical downwards, in kilometers. The data of the model region have dimensions of 1800×800×400 km (length×width×depth). The geometry of the subducted plate is well constrained by Slab2.0, and the plate ages are provided by EarthByte. The temperature boundary condition agrees with the plate cooling model. The bottom of the slab and the perpendicular plane are prescribed as adiabatic and permeable, and the top surface is set to a fixed temperature (0°C) and is rigid. The data was acquired through 3-D numerical thermal modeling which was developed from originally code stag3d. An anelastic liquid approximation and the equations of conservation of mass, momentum, and energy are used in this model. Based on a three-dimensional thermomechanical model and the collect earthquake catalog from IRIS, the data of the slab thermal state, water content, and slab dehydration distribution in Kuril-Kamchatka are calculated. THIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE. TO VIEW A LIST OF FILES AND ACCESS THE FILES IN THIS DATASET CLICK ON THE DOI-LINK ABOVE Other/Unknown Material Kamchatka Data Archiving and Networked Services (DANS): EASY (KNAW - Koninklijke Nederlandse Akademie van Wetenschappen) The ''Y'' ENVELOPE(-112.453,-112.453,57.591,57.591) |
institution |
Open Polar |
collection |
Data Archiving and Networked Services (DANS): EASY (KNAW - Koninklijke Nederlandse Akademie van Wetenschappen) |
op_collection_id |
ftdans |
language |
unknown |
topic |
Interdisciplinary sciences |
spellingShingle |
Interdisciplinary sciences Ji, Y (via Mendeley Data) 3-D thermal regime and petrologic metamorphism in Kuril-Kamchatka |
topic_facet |
Interdisciplinary sciences |
description |
The data include the 3-D temperature field (degrees Celsius), water content (wt%), dehydration rate (wt%/km), and subduction velocity field (cm/yr) of the subducting plate, as well as the coastline and volcano distribution in Kuril-Kamchatka. The data coordinates are an orthogonal coordinate system, where the origin of the coordinates is (156.00E,47.18N), the x+ azimuth is 133 degrees clockwise from the north, and the y+ azimuth is 43 degrees clockwise from the north, and the z+ direction is vertical downwards, in kilometers. The data of the model region have dimensions of 1800×800×400 km (length×width×depth). The geometry of the subducted plate is well constrained by Slab2.0, and the plate ages are provided by EarthByte. The temperature boundary condition agrees with the plate cooling model. The bottom of the slab and the perpendicular plane are prescribed as adiabatic and permeable, and the top surface is set to a fixed temperature (0°C) and is rigid. The data was acquired through 3-D numerical thermal modeling which was developed from originally code stag3d. An anelastic liquid approximation and the equations of conservation of mass, momentum, and energy are used in this model. Based on a three-dimensional thermomechanical model and the collect earthquake catalog from IRIS, the data of the slab thermal state, water content, and slab dehydration distribution in Kuril-Kamchatka are calculated. THIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE. TO VIEW A LIST OF FILES AND ACCESS THE FILES IN THIS DATASET CLICK ON THE DOI-LINK ABOVE |
author |
Ji, Y (via Mendeley Data) |
author_facet |
Ji, Y (via Mendeley Data) |
author_sort |
Ji, Y (via Mendeley Data) |
title |
3-D thermal regime and petrologic metamorphism in Kuril-Kamchatka |
title_short |
3-D thermal regime and petrologic metamorphism in Kuril-Kamchatka |
title_full |
3-D thermal regime and petrologic metamorphism in Kuril-Kamchatka |
title_fullStr |
3-D thermal regime and petrologic metamorphism in Kuril-Kamchatka |
title_full_unstemmed |
3-D thermal regime and petrologic metamorphism in Kuril-Kamchatka |
title_sort |
3-d thermal regime and petrologic metamorphism in kuril-kamchatka |
publishDate |
2022 |
url |
http://nbn-resolving.org/urn:nbn:nl:ui:13-ym-ennn https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:260627 |
long_lat |
ENVELOPE(-112.453,-112.453,57.591,57.591) |
geographic |
The ''Y'' |
geographic_facet |
The ''Y'' |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_relation |
2 jgy68s9ttg http://nbn-resolving.org/urn:nbn:nl:ui:13-ym-ennn doi:10.17632/jgy68s9ttg.2 https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:260627 |
op_rights |
OPEN_ACCESS: The data are archived in Easy, they are accessible elsewhere through the DOI https://dans.knaw.nl/en/about/organisation-and-policy/legal-information/DANSLicence.pdf Yingfeng Ji |
op_doi |
https://doi.org/10.17632/jgy68s9ttg.2 |
_version_ |
1770272485510479872 |