Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures

Summary: Previous subduction thermal models are inconsistent with the values of forearc heat flow (50–140 mW/m2) and global P‒T conditions of exhumed rocks, both suggesting a shallow environment 200–300°C warmer than model predictions. Here, we revaluate these problems in Kuril-Kamchatka using 3D th...

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Published in:iScience
Main Authors: Weiling Zhu, Yingfeng Ji, Lijun Liu, Rui Qu, Ye Zhu, Chaodi Xie, Lin Ding
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2023
Subjects:
Q
Online Access:https://doi.org/10.1016/j.isci.2023.107288
https://doaj.org/article/3240fb53c27f4f2f92bb1c4826d65abb
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spelling ftdoajarticles:oai:doaj.org/article:3240fb53c27f4f2f92bb1c4826d65abb 2023-08-20T04:07:39+02:00 Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures Weiling Zhu Yingfeng Ji Lijun Liu Rui Qu Ye Zhu Chaodi Xie Lin Ding 2023-08-01T00:00:00Z https://doi.org/10.1016/j.isci.2023.107288 https://doaj.org/article/3240fb53c27f4f2f92bb1c4826d65abb EN eng Elsevier http://www.sciencedirect.com/science/article/pii/S2589004223013652 https://doaj.org/toc/2589-0042 2589-0042 doi:10.1016/j.isci.2023.107288 https://doaj.org/article/3240fb53c27f4f2f92bb1c4826d65abb iScience, Vol 26, Iss 8, Pp 107288- (2023) Earth sciences Geology Tectonics Science Q article 2023 ftdoajarticles https://doi.org/10.1016/j.isci.2023.107288 2023-07-30T00:40:17Z Summary: Previous subduction thermal models are inconsistent with the values of forearc heat flow (50–140 mW/m2) and global P‒T conditions of exhumed rocks, both suggesting a shallow environment 200–300°C warmer than model predictions. Here, we revaluate these problems in Kuril-Kamchatka using 3D thermomechanical modeling that satisfies the observed subduction history and slab geometry, while our refined 3D slab thermal state is warmer than that predicted by previous 2D models and better matches observational constraints. We show that warmer slabs create hierarchical slab dehydration fronts at various forearc depths, causing fast and slow subduction earthquakes. We conclude that fast-to-slow subduction earthquakes all play a key role in balancing plate coupling energy release on megathrusts trenchward of high P-T volcanism. Article in Journal/Newspaper Kamchatka Directory of Open Access Journals: DOAJ Articles iScience 26 8 107288
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Earth sciences
Geology
Tectonics
Science
Q
spellingShingle Earth sciences
Geology
Tectonics
Science
Q
Weiling Zhu
Yingfeng Ji
Lijun Liu
Rui Qu
Ye Zhu
Chaodi Xie
Lin Ding
Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures
topic_facet Earth sciences
Geology
Tectonics
Science
Q
description Summary: Previous subduction thermal models are inconsistent with the values of forearc heat flow (50–140 mW/m2) and global P‒T conditions of exhumed rocks, both suggesting a shallow environment 200–300°C warmer than model predictions. Here, we revaluate these problems in Kuril-Kamchatka using 3D thermomechanical modeling that satisfies the observed subduction history and slab geometry, while our refined 3D slab thermal state is warmer than that predicted by previous 2D models and better matches observational constraints. We show that warmer slabs create hierarchical slab dehydration fronts at various forearc depths, causing fast and slow subduction earthquakes. We conclude that fast-to-slow subduction earthquakes all play a key role in balancing plate coupling energy release on megathrusts trenchward of high P-T volcanism.
format Article in Journal/Newspaper
author Weiling Zhu
Yingfeng Ji
Lijun Liu
Rui Qu
Ye Zhu
Chaodi Xie
Lin Ding
author_facet Weiling Zhu
Yingfeng Ji
Lijun Liu
Rui Qu
Ye Zhu
Chaodi Xie
Lin Ding
author_sort Weiling Zhu
title Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures
title_short Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures
title_full Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures
title_fullStr Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures
title_full_unstemmed Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures
title_sort reestimation of slab dehydration fronts in kuril-kamchatka using updated global subduction zone thermal structures
publisher Elsevier
publishDate 2023
url https://doi.org/10.1016/j.isci.2023.107288
https://doaj.org/article/3240fb53c27f4f2f92bb1c4826d65abb
genre Kamchatka
genre_facet Kamchatka
op_source iScience, Vol 26, Iss 8, Pp 107288- (2023)
op_relation http://www.sciencedirect.com/science/article/pii/S2589004223013652
https://doaj.org/toc/2589-0042
2589-0042
doi:10.1016/j.isci.2023.107288
https://doaj.org/article/3240fb53c27f4f2f92bb1c4826d65abb
op_doi https://doi.org/10.1016/j.isci.2023.107288
container_title iScience
container_volume 26
container_issue 8
container_start_page 107288
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