Delaminated lower slab thermal regime before slab break-off in the Pamirs:Implications from 3D kinematic modelingOA
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
State Key Laboratory of Tibetan Plateau Earth System,Environment and Resources(TPESER),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,ChinaUniversity of Chinese Academy of Sciences,Beijing 100049,ChinaState Key Laboratory of Tibetan Plateau Earth System,Environment and Resources(TPESER),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,ChinaUniversity of Chinese Academy of Sciences,Beijing 100049,ChinaState Key Laboratory of Tibetan Plateau Earth System,Environment and Resources(TPESER),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,ChinaUniversity of Chinese Academy of Sciences,Beijing 100049,ChinaState Key Laboratory of Tibetan Plateau Earth System,Environment and Resources(TPESER),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,ChinaUniversity of Chinese Academy of Sciences,Beijing 100049,ChinaState Key Laboratory of Tibetan Plateau Earth System,Environment and Resources(TPESER),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China
Pamirssubduction3D kinematic modelingslab geometryintermediate-depth earthquakecrustal delaminationseismicity distribution
Pamirssubduction3D kinematic modelingslab geometryintermediate-depth earthquakecrustal delaminationseismicity distribution
《地球与行星物理（英文）》 2026 (1)
13-21,9
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.
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