Deep-Time Source-to-Sink in Continental Basins

A special issue of Minerals (ISSN 2075-163X).

Deadline for manuscript submissions: 31 October 2025 | Viewed by 693

Special Issue Editors


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Guest Editor
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
Interests: sedimentology; tectonic-climatic event; seismic interpretation

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Guest Editor
School of Ocean Sciences, China University of Geosciences-Beijing, Beijing 100023, China
Interests: sediment routings; detrital zircons; volcanism

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Guest Editor
College of Oceanography , Hohai Univeirsity, Nanjing 210098, China
Interests: sequence stratigraphy; sedimentology; basin analysis

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Guest Editor
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
Interests: sequence stratigraphy; seismic sedimentology; source-to-sink

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Guest Editor
College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China
Interests: sedimentology; seismic sedimentology; sequence stratigraphy
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Special Issue Information

Dear Colleagues,

The deep-time source-to-sink system in continental basins is a cutting-edge research topic in sedimentology and has been attempted by building on the research experience of the Quaternary ocean land margins. The multifactor configuration link between provenance signals, geomorphological elements, and sedimentary records is mostly described in terms of weathering, denudation, transportation, and the accumulation of detrital particles. Key geologic issues are then 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 is proposed that potential innovations might emerge from the research fields of tectonism–climate-regulated weathering efficacy, the relationship between catchment geomorphology and sediment supply, the prediction of sediment routing system interaction models, paleo-water depth-hydrodynamics constraints on sandstone dispersal, forward modeling to restore source-to-sink processes, and so on. By doing so, it is hoped that the problems of sediment flux pickup and balance restoration under the influence of multiple driving factors and interacting media in the deep-time continental basins can be effectively solved.

This Special Issue aims to provide an overview of the latest research, methodologies, and case studies on the deep-time continental source-to-sink systems. We welcome the submission of high-quality, original research papers that address the following topics:

  • Section 1: source-to-sink systems of continental basin—case studies of drainage basin geomorphological analysis, sediment flux variation, and coupling of sedimentary responses in source-to-sink systems in different types of continental basins (including rift, foreland, or cratonic basin).
  • Section 2: sediment routing reconstruction—qualitative/quantitative methods and case studies of sediment routing analysis, using petrological, mineralogical, geochronology, geochemical, forward modeling, machine learning techniques, etc.
  • Section 3: paleoclimate and aquatic environment reconstruction—to investigate how palaeoclimate and signals from aquatic environments (including chemical solution) affect the effectiveness of sediment weathering and dispersal mechanisms.

Dr. Qianghu Liu
Dr. Hehe Chen
Dr. Mingxuan Tan
Prof. Dr. Hongtao Zhu
Prof. Dr. Xiaomin Zhu
Guest Editors

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Keywords

  • deep-time source-to-sink system
  • catchment geomorphology
  • sediment routings
  • sediment flux
  • sedimentary response
  • detrital zircons
  • forward modeling
  • deep-time digital earth

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Published Papers (1 paper)

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Research

30 pages, 18951 KiB  
Article
Identification and Sedimentary Model of Shallow-Water Deltas: A Case Study of the Funing Formation, Subei Basin, Northeast China
by Ziyi Yang, Guiyu Dong, Lianbo Zeng, Yongfeng Qiu, Chen Guo, Zhao Ma, Tianwei Wang, Xu Yang, Shuo Ran and Xing Zhao
Minerals 2025, 15(3), 207; https://doi.org/10.3390/min15030207 - 21 Feb 2025
Viewed by 302
Abstract
Shallow-water deltas are not only a hot spot for sedimentological research but also a key target for oil and gas exploration. In this paper, taking the third member (E1f3) of the Funing Formation in the Upper Jurassic as an [...] Read more.
Shallow-water deltas are not only a hot spot for sedimentological research but also a key target for oil and gas exploration. In this paper, taking the third member (E1f3) of the Funing Formation in the Upper Jurassic as an example, based on observations made from core samples, well logging, cathode luminescence characteristics, and analytical assays, the development conditions, sedimentary characteristics, and sedimentary models of shallow-water deltas are summarized. These shallow-water deltas were deposited in conditions with the following characteristics: a gentle terrain platform, a subtropical climate with ample rainfall, an abundant source supply, strong hydrodynamic forces, shallow water bodies, and a frequently eustatic lake level. Shallow-water deltas are characterized by sediment deposition from traction currents, numerous underwater distributary channel scour structures, overlapping scouring structures, sand body distribution with planar features, underwater distributary channels as skeletal sand bodies, and undeveloped mouth bars. Based on these, it is believed that during the deposition period of E1f3, the Gaoyou Sag in the Subei Basin had favorable geological conditions for the development of shallow-water delta deposition. The shallow-water delta deposition that occurred during the sedimentary periods of the five major sand units in the Funing Formation is characterized by front subfacies, with underwater distributary channels as the framework for sand bodies, and multiple intermittent positive rhythms overlapping vertically with the Jianhu Uplift as the source of material supply. In this paper, a depositional model for shallow-water delta deposition during the E1f3 deposition period in the Gaoyou Sag is established, expanding the scope of oil reservoir exploration in the north slope region of the Gaoyou Sag and providing important geological evidence for the selection of favorable subtle zones. Full article
(This article belongs to the Special Issue Deep-Time Source-to-Sink in Continental Basins)
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