Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet

A new technique for P-wave receiver function (PRF) inversion, within the framework of wave equation-based adjoint tomography and referred to as receiver function adjoint tomography (RFAT), has been developed to obtain models of Vp, Vs, and density. This innovative technique fits the synthetic PRFs w...

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Main Authors: Xu, Mijian, Wang, Kai, Chen, Jing, Yu, Dayong, Tong, Ping
Other Authors: Asian School of the Environment
Format: Article
Language:English
Published: 2024
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Online Access:https://hdl.handle.net/10356/173111
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-1731112024-01-15T15:30:44Z Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet Xu, Mijian Wang, Kai Chen, Jing Yu, Dayong Tong, Ping Asian School of the Environment School of Physical and Mathematical Sciences Earth Observatory of Singapore Science::Geology Science::Physics Image Resolution P-wave A new technique for P-wave receiver function (PRF) inversion, within the framework of wave equation-based adjoint tomography and referred to as receiver function adjoint tomography (RFAT), has been developed to obtain models of Vp, Vs, and density. This innovative technique fits the synthetic PRFs with observed PRFs and can better image the lateral variations of Vs from the crust to the uppermost mantle than traditional 1-D PRF inversion. We utilized RFAT to perform high-resolution imaging beneath a dense seismic array in Southeastern Tibet, revealing low-velocity zones extending from the uppermost mantle to the crust, as well as an eastward dipping Moho under the Red River Fault (RRF). Our inversion results provide direct evidence for the existence of a distinct asthenospheric upwelling channel beneath the RRF, and further highlight the effectiveness of RFAT for accurately imaging subsurface structures. Ministry of Education (MOE) National Research Foundation (NRF) Published version This study was supported by the Ministry of Educa-tion, Singapore, under its MOE AcRF Tier 2_February 2022 Grant Call (MOE-T2EP20122-0008). MX, KW and PT were partially supported by the National Research Foundation Singapore and Singapore Ministry of Education under the Research Centers of Excel-lence Initiative (04MNS001913A620). This study was also funded by the National Key R&D Program of China (2016YFC0600302). 2024-01-12T06:15:37Z 2024-01-12T06:15:37Z 2023 Journal Article Xu, M., Wang, K., Chen, J., Yu, D. & Tong, P. (2023). Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet. Geophysical Research Letters, 50(19), e2023GL104077-. https://dx.doi.org/10.1029/2023GL104077 0094-8276 https://hdl.handle.net/10356/173111 10.1029/2023GL104077 2-s2.0-85173569822 19 50 e2023GL104077 en MOE-T2EP20122-0008 04MNS001913A620 Geophysical Research Letters © 2023 The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made. application/pdf
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Science::Geology
Science::Physics
Image Resolution
P-wave
spellingShingle Science::Geology
Science::Physics
Image Resolution
P-wave
Xu, Mijian
Wang, Kai
Chen, Jing
Yu, Dayong
Tong, Ping
Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet
description A new technique for P-wave receiver function (PRF) inversion, within the framework of wave equation-based adjoint tomography and referred to as receiver function adjoint tomography (RFAT), has been developed to obtain models of Vp, Vs, and density. This innovative technique fits the synthetic PRFs with observed PRFs and can better image the lateral variations of Vs from the crust to the uppermost mantle than traditional 1-D PRF inversion. We utilized RFAT to perform high-resolution imaging beneath a dense seismic array in Southeastern Tibet, revealing low-velocity zones extending from the uppermost mantle to the crust, as well as an eastward dipping Moho under the Red River Fault (RRF). Our inversion results provide direct evidence for the existence of a distinct asthenospheric upwelling channel beneath the RRF, and further highlight the effectiveness of RFAT for accurately imaging subsurface structures.
author2 Asian School of the Environment
author_facet Asian School of the Environment
Xu, Mijian
Wang, Kai
Chen, Jing
Yu, Dayong
Tong, Ping
format Article
author Xu, Mijian
Wang, Kai
Chen, Jing
Yu, Dayong
Tong, Ping
author_sort Xu, Mijian
title Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet
title_short Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet
title_full Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet
title_fullStr Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet
title_full_unstemmed Receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in Southeastern Tibet
title_sort receiver function adjoint tomography for three-dimensional high-resolution seismic array imaging: methodology and applications in southeastern tibet
publishDate 2024
url https://hdl.handle.net/10356/173111
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