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首页|期刊导航|中国海洋大学学报(自然科学英文版)|Stratigraphic Forward Modeling of Late Quaternary Fluvial Dynamics in the Indus River Delta,Pakistan:Insights into Sea Level-Driven Sedimentary Evolution

Stratigraphic Forward Modeling of Late Quaternary Fluvial Dynamics in the Indus River Delta,Pakistan:Insights into Sea Level-Driven Sedimentary Evolution

HASSAN Hafiz Ahmed Raza LIU Keyu LIU Jianliang MUNAWAR Muhammad Jawad REHMAN Saif Ur HUSSAIN Abid

中国海洋大学学报(自然科学英文版)2025,Vol.24Issue(6):1500-1518,19.
中国海洋大学学报(自然科学英文版)2025,Vol.24Issue(6):1500-1518,19.DOI:10.1007/s11802-025-6075-9

Stratigraphic Forward Modeling of Late Quaternary Fluvial Dynamics in the Indus River Delta,Pakistan:Insights into Sea Level-Driven Sedimentary Evolution

Stratigraphic Forward Modeling of Late Quaternary Fluvial Dynamics in the Indus River Delta,Pakistan:Insights into Sea Level-Driven Sedimentary Evolution

HASSAN Hafiz Ahmed Raza 1LIU Keyu 2LIU Jianliang 1MUNAWAR Muhammad Jawad 3REHMAN Saif Ur 3HUSSAIN Abid4

作者信息

  • 1. State Key Laboratory of Deep Oil and Gas,China University of Petroleum(East China),Qingdao 266580,China
  • 2. State Key Laboratory of Deep Oil and Gas,China University of Petroleum(East China),Qingdao 266580,China||Laboratory for Marine Mineral Resource Evaluation and Exploration,Laoshan Laboratory,Qingdao 266071,China
  • 3. Institute of Geology,University of the Punjab,Lahore 54590,Pakistan
  • 4. Mari Energies Limited,Islamabad 44000,Pakistan
  • 折叠

摘要

关键词

fluvial responses/sea level changes/glacial-interglacial cycle/sedimentary evolution/stratigraphic forward modeling/Indus Delta

Key words

fluvial responses/sea level changes/glacial-interglacial cycle/sedimentary evolution/stratigraphic forward modeling/Indus Delta

引用本文复制引用

HASSAN Hafiz Ahmed Raza,LIU Keyu,LIU Jianliang,MUNAWAR Muhammad Jawad,REHMAN Saif Ur,HUSSAIN Abid..Stratigraphic Forward Modeling of Late Quaternary Fluvial Dynamics in the Indus River Delta,Pakistan:Insights into Sea Level-Driven Sedimentary Evolution[J].中国海洋大学学报(自然科学英文版),2025,24(6):1500-1518,19.

基金项目

This research is funded by the Science and Technology Innovation Project of the Laoshan Laboratory(No.LSKJ202203402),and the Major Research Project on the Tethys Geodynamic System from the National Science Foundation of China(No.92055204).China University of Petroleum,Qingdao,is gratefully acknowledged for pro-viding research facilities and a scholarship to the lead au-thor. (No.LSKJ202203402)

中国海洋大学学报(自然科学英文版)

1672-5182

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