辫曲转换与共存的主要影响因素及对古代河流沉积环境恢复的启示

李胜利; 马水平; 周练武; 黄晓娣; 韩波; 李航

doi:10.3799/dqkx.2022.013

Volume 47 Issue 11

Nov. 2022

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Article Navigation > Earth Science > 2022 > 47(11): 3960-3976

Li Shengli, Ma Shuiping, Zhou Lianwu, Huang Xiaodi, Han Bo, Li Hang, 2022. Main Influencing Factors of Braided-Meander Transition and Coexistence Characteristics and Implications of Ancient Fluvial Sedimentary Environment Reconstruction. Earth Science, 47(11): 3960-3976. doi: 10.3799/dqkx.2022.013

Citation:

Li Shengli, Ma Shuiping, Zhou Lianwu, Huang Xiaodi, Han Bo, Li Hang, 2022. Main Influencing Factors of Braided-Meander Transition and Coexistence Characteristics and Implications of Ancient Fluvial Sedimentary Environment Reconstruction. Earth Science, 47(11): 3960-3976. doi: 10.3799/dqkx.2022.013

Citation:

Li Shengli, Ma Shuiping, Zhou Lianwu, Huang Xiaodi, Han Bo, Li Hang, 2022. Main Influencing Factors of Braided-Meander Transition and Coexistence Characteristics and Implications of Ancient Fluvial Sedimentary Environment Reconstruction. Earth Science, 47(11): 3960-3976. doi: 10.3799/dqkx.2022.013

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Main Influencing Factors of Braided-Meander Transition and Coexistence Characteristics and Implications of Ancient Fluvial Sedimentary Environment Reconstruction

doi: 10.3799/dqkx.2022.013

1.
Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism, Ministry of Education, School of Energy Resources, China University of Geosciences, Beijing 100083, China
2.
No.2 Production Plant of Dagang Oilfield Company, Tianjin 061108, China

Received Date: 2022-01-02
Available Online: 2022-12-07
Publish Date: 2022-11-25

Abstract

Abstract

The braided-meander transition and coexistence phenomenon is a hot issue in physical geography, hydraulics and fluvial sedimentary geology. It also has important reference significance for ancient fluvial sedimentary environment reconstruction and reservoir prediction. Firstly, it discusses the main influencing factors of the characteristics of fluvial braided-meander transition and coexistence, and points out that the main factors such as structural change and geomorphic unit, the difference of slope gradient, the distance of provenance and hydrodynamic conditions, climate change and vegetation development, sea/lake level change control the process of braid river type transformation. Among them, tectonic change and geomorphic unit are the key factors. Then, four implications of the concept of braided-meander transition on the study of ancient river sedimentary facies reconstruction are summarized. Taking the Lower Shihezi Formation in the lower part of the Middle Permian in Daniudi gas field, Ordos basin, as an example, combined with the characteristics of well-logging curves, seismic attributes and sandstone thickness distribution law, the concept of braided-meander transition and coexistence was applied to the reconstruction of ancient fluvial environment. Finally, fluvial sedimentary distribution pattern of H2¹ sand bed in the gas field area was reconstructed. It is indicated that braided river prevailed in the northern part and meandering river was mainly developed in the southern part in the gas field area. It is pointed out that it is easier to form abandoned river channels in the braided-meander zone and the adjacent meandering river area.

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Main Influencing Factors of Braided-Meander Transition and Coexistence Characteristics and Implications of Ancient Fluvial Sedimentary Environment Reconstruction

doi: 10.3799/dqkx.2022.013

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通讯作者: 陈斌, bchen63@163.com

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