Numerical modeling the process of deep slab dehydration and magmatism

Abstract This study uses a 2D high-resolution thermo-mechanical coupled model to investigate the dynamic processes of deep plate hydration, dehydration, and subsequent magmatic activity in ocean-continent subduction zones. We reveal the pathways and temporal evolution of water transport to the deep...

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Main Authors: Hao Wu, Jiacheng Lei, Zeyu Jia, Jian Sheng, Yinan Zhu, Jian Wang
Format: Article
Language:English
Published: Nature Portfolio 2024-11-01
Series:Scientific Reports
Subjects:
Online Access:https://doi.org/10.1038/s41598-024-78193-w
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author Hao Wu
Jiacheng Lei
Zeyu Jia
Jian Sheng
Yinan Zhu
Jian Wang
author_facet Hao Wu
Jiacheng Lei
Zeyu Jia
Jian Sheng
Yinan Zhu
Jian Wang
author_sort Hao Wu
collection DOAJ
description Abstract This study uses a 2D high-resolution thermo-mechanical coupled model to investigate the dynamic processes of deep plate hydration, dehydration, and subsequent magmatic activity in ocean-continent subduction zones. We reveal the pathways and temporal evolution of water transport to the deep mantle during the subduction process. Plate dehydration plays a critical role in triggering partial melting of the deep mantle and related magmatic activity. Our study shows significant differences in the volumes of melt produced at different depths, with dehydration reactions in deeper regions being weaker compared to shallower ones. It takes a longer time to reach the suitable P-T conditions for hydrous melting in the deep mantle. The results highlight the geophysical significance of water transport in deep subduction zones and its role in magmatic processes, particularly in the formation of magma chambers beneath continental plates.
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institution Kabale University
issn 2045-2322
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publishDate 2024-11-01
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spelling doaj-art-d12be5f85ac94115b31213fb4fe5d7692025-01-12T12:25:16ZengNature PortfolioScientific Reports2045-23222024-11-0114111710.1038/s41598-024-78193-wNumerical modeling the process of deep slab dehydration and magmatismHao Wu0Jiacheng Lei1Zeyu Jia 2Jian Sheng3Yinan Zhu4Jian Wang5College of Transportation Engineering of Nanjing Tech, Nanjing Tech UniversityCollege of Transportation Engineering of Nanjing Tech, Nanjing Tech UniversityCollege of Transportation Engineering of Nanjing Tech, Nanjing Tech UniversityCollege of Transportation Engineering of Nanjing Tech, Nanjing Tech UniversityCollege of Transportation Engineering of Nanjing Tech, Nanjing Tech UniversityCollege of Transportation Engineering of Nanjing Tech, Nanjing Tech UniversityAbstract This study uses a 2D high-resolution thermo-mechanical coupled model to investigate the dynamic processes of deep plate hydration, dehydration, and subsequent magmatic activity in ocean-continent subduction zones. We reveal the pathways and temporal evolution of water transport to the deep mantle during the subduction process. Plate dehydration plays a critical role in triggering partial melting of the deep mantle and related magmatic activity. Our study shows significant differences in the volumes of melt produced at different depths, with dehydration reactions in deeper regions being weaker compared to shallower ones. It takes a longer time to reach the suitable P-T conditions for hydrous melting in the deep mantle. The results highlight the geophysical significance of water transport in deep subduction zones and its role in magmatic processes, particularly in the formation of magma chambers beneath continental plates.https://doi.org/10.1038/s41598-024-78193-wPlate dehydrationMagmatic activityDeep subduction zoneMantle meltinMagma chamber formation
spellingShingle Hao Wu
Jiacheng Lei
Zeyu Jia
Jian Sheng
Yinan Zhu
Jian Wang
Numerical modeling the process of deep slab dehydration and magmatism
Scientific Reports
Plate dehydration
Magmatic activity
Deep subduction zone
Mantle meltin
Magma chamber formation
title Numerical modeling the process of deep slab dehydration and magmatism
title_full Numerical modeling the process of deep slab dehydration and magmatism
title_fullStr Numerical modeling the process of deep slab dehydration and magmatism
title_full_unstemmed Numerical modeling the process of deep slab dehydration and magmatism
title_short Numerical modeling the process of deep slab dehydration and magmatism
title_sort numerical modeling the process of deep slab dehydration and magmatism
topic Plate dehydration
Magmatic activity
Deep subduction zone
Mantle meltin
Magma chamber formation
url https://doi.org/10.1038/s41598-024-78193-w
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