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首页|期刊导航|地球与行星物理(英文)|Delaminated lower slab thermal regime before slab break-off in the Pamirs:Implications from 3D kinematic modeling

Delaminated lower slab thermal regime before slab break-off in the Pamirs:Implications from 3D kinematic modeling

Haris Faheem YingFeng Ji Waqar Ahmed Rui Qu Ye Zhu Fitriani Fitriani Jun Yang Shoichi Yoshioka Nobuaki Suenaga

地球与行星物理(英文)2026,Vol.10Issue(1):13-21,9.
地球与行星物理(英文)2026,Vol.10Issue(1):13-21,9.DOI:10.26464/epp2026012

Delaminated lower slab thermal regime before slab break-off in the Pamirs:Implications from 3D kinematic modeling

Delaminated lower slab thermal regime before slab break-off in the Pamirs:Implications from 3D kinematic modeling

Haris Faheem 1YingFeng Ji 2Waqar Ahmed 1Rui Qu 2Ye Zhu 1Fitriani Fitriani 2Jun Yang 1Shoichi Yoshioka 2Nobuaki Suenaga1

作者信息

  • 1. State Key Laboratory of Tibetan Plateau Earth System,Environment and Resources(TPESER),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China
  • 2. University of Chinese Academy of Sciences,Beijing 100049,China
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摘要

关键词

Pamirs/subduction/3D kinematic modeling/slab geometry/intermediate-depth earthquake/crustal delamination/seismicity distribution

Key words

Pamirs/subduction/3D kinematic modeling/slab geometry/intermediate-depth earthquake/crustal delamination/seismicity distribution

引用本文复制引用

Haris Faheem,YingFeng Ji,Waqar Ahmed,Rui Qu,Ye Zhu,Fitriani Fitriani,Jun Yang,Shoichi Yoshioka,Nobuaki Suenaga..Delaminated lower slab thermal regime before slab break-off in the Pamirs:Implications from 3D kinematic modeling[J].地球与行星物理(英文),2026,10(1):13-21,9.

基金项目

This study benefited from the financial support of the Chinese Academy of Sciences Pioneer Hundred Talents Program and the Second Tibetan Plateau Scientific Expedition and Research Program(Grant No.2019QZKK0708).This work was partly supported by a MEXT(Ministry of Education,Culture,Sports,Science and Technology)KAKENHI(Grants-in-Aid for Scientific Research)grant(Grant No.21H05203)and Kobe University Strategic International Collaborative Research Grant(Type B Fostering Joint Research).We thank P.Tackley for sharing the original Stage3D code that was used in our study.Figures were created via Generic Mapping Tools and ParaView software developed by Kitware,Inc.We also gained knowledge through the support of computing facilities provided by the Institute of Tibetan Plateau Research,including the Sugon supercomputing platform and workstations. (Grant No.2019QZKK0708)

地球与行星物理(英文)

2096-3955

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