陆相裂陷盆地深时源-汇系统关键地质问题及革新方向

刘强虎; 李志垚; 陈贺贺; 周子强; 谈明轩; 朱筱敏

doi:10.3799/dqkx.2023.194

Volume 48 Issue 12

Dec. 2023

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Article Navigation > Earth Science > 2023 > 48(12): 4586-4612

Liu Qianghu, Li Zhiyao, Chen Hehe, Zhou Ziqiang, Tan Mingxuan, Zhu Xiaomin, 2023. Key Geological Issues and Innovation Directions in Deep-Time Source-to-Sink System of Continental Rift Basins. Earth Science, 48(12): 4586-4612. doi: 10.3799/dqkx.2023.194

Citation:

Liu Qianghu, Li Zhiyao, Chen Hehe, Zhou Ziqiang, Tan Mingxuan, Zhu Xiaomin, 2023. Key Geological Issues and Innovation Directions in Deep-Time Source-to-Sink System of Continental Rift Basins. Earth Science, 48(12): 4586-4612. doi: 10.3799/dqkx.2023.194

Citation:

Liu Qianghu, Li Zhiyao, Chen Hehe, Zhou Ziqiang, Tan Mingxuan, Zhu Xiaomin, 2023. Key Geological Issues and Innovation Directions in Deep-Time Source-to-Sink System of Continental Rift Basins. Earth Science, 48(12): 4586-4612. doi: 10.3799/dqkx.2023.194

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Key Geological Issues and Innovation Directions in Deep-Time Source-to-Sink System of Continental Rift Basins

doi: 10.3799/dqkx.2023.194

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Sciences, Zhejiang University, Hangzhou 310058, China
3.
School of Ocean Sciences, China University of Geosciences, Beijing 100083, China
4.
School of Earth Science and Engineering, Imperial College London, London SW72AZ, United Kingdom
5.
School of Ocean Sciences, Hohai University, Nanjing 210098, China
6.
College of Geosciences, China University of Petroleum, Beijing 102249, China

Received Date: 2023-07-11
Publish Date: 2023-12-25

Abstract

Abstract

The deep-time source-to-sink system in continental rift basins is a cutting-edge research topic in sedimentology and has been attempted by building on the research experience on the Quaternary ocean-land margins. Four key geological issues are raised, namely the research scale or level of the source-to-sink system, geomorphologic evolution and sediment output in the catchment, signal propagation and modification through the sediment routing system, and multifactorial joint control of sedimentary-stratigraphic development in the basin. In light of these issues, it proposes that the potential innovations might emerge from the research fields of volcanism-modified sedimentary sequences, palaeoclimate-vegetation community-regulated weathering efficacy, the relationship between catchment geomorphology and sediment supply, prediction of sediment routing system interaction models, paleo water depth-hydrodynamics constraints on sandstone dispersal, forward modeling to restore source-to-sink processes, and source-to-sink response of carbonate dissolved matter. By doing so, it hopes that the problems of sediment-flux pickup and balance restoration under the influence of multiple driving factors and interacting media in the continental deep-time rift basins can be effectively solved. In addition, it suggests that multi-disciplinary cross-integration and multi-element construction of deep-time big data system are two key directions for expanding the research connotation of continental deep-time source-to-sink system with Chinese characteristic and serving the exploration and prediction of energy minerals.
- continental deep-time source-to-sink system,
- landform,
- sediment signal,
- paleoclimate-water environment,
- big data,
- key geological issue,
- innovation directions,
- sedimentology

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References(229)

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