Weak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the Longmenshan area, China
Abstract A large amount of high-quality teleseismic data is used for common conversion point (CCP) stacking of receiver functions in the Longmenshan area and near-by region. The results show that a large-scale high-velocity anomaly (LHVA) or lithospheric delamination can modify the structure of uppe...
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2021
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oai:doaj.org-article:5c2148847b1f47369d44b86b9d0da6322021-11-08T10:49:21ZWeak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the Longmenshan area, China10.1038/s41598-021-01061-42045-2322https://doaj.org/article/5c2148847b1f47369d44b86b9d0da6322021-11-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-01061-4https://doaj.org/toc/2045-2322Abstract A large amount of high-quality teleseismic data is used for common conversion point (CCP) stacking of receiver functions in the Longmenshan area and near-by region. The results show that a large-scale high-velocity anomaly (LHVA) or lithospheric delamination can modify the structure of upper mantle discontinuities or weaken the phase boundary of olivine, which is a very important finding and can be used to assess stagnant slabs in the mantle transition zone globally. The deepening region of the 660 km discontinuity beneath the Songpan-Ganzi terrane identified in this study might be generated by the LHVA.Chuansong HeNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-7 (2021) |
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Medicine R Science Q Chuansong He Weak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the Longmenshan area, China |
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Abstract A large amount of high-quality teleseismic data is used for common conversion point (CCP) stacking of receiver functions in the Longmenshan area and near-by region. The results show that a large-scale high-velocity anomaly (LHVA) or lithospheric delamination can modify the structure of upper mantle discontinuities or weaken the phase boundary of olivine, which is a very important finding and can be used to assess stagnant slabs in the mantle transition zone globally. The deepening region of the 660 km discontinuity beneath the Songpan-Ganzi terrane identified in this study might be generated by the LHVA. |
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article |
author |
Chuansong He |
author_facet |
Chuansong He |
author_sort |
Chuansong He |
title |
Weak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the Longmenshan area, China |
title_short |
Weak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the Longmenshan area, China |
title_full |
Weak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the Longmenshan area, China |
title_fullStr |
Weak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the Longmenshan area, China |
title_full_unstemmed |
Weak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the Longmenshan area, China |
title_sort |
weak and vanishing upper mantle discontinuities generated by large-scale lithospheric delamination in the longmenshan area, china |
publisher |
Nature Portfolio |
publishDate |
2021 |
url |
https://doaj.org/article/5c2148847b1f47369d44b86b9d0da632 |
work_keys_str_mv |
AT chuansonghe weakandvanishinguppermantlediscontinuitiesgeneratedbylargescalelithosphericdelaminationinthelongmenshanareachina |
_version_ |
1718442619412938752 |