渤海海域南部古水系恢复及其沉积耦合响应预测

石文龙; 杨海风; 杜晓峰; 高雁飞; 刘睿; 涂翔

doi:10.3799/dqkx.2022.022

Volume 47 Issue 11

Nov. 2022

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Article Navigation > Earth Science > 2022 > 47(11): 4075-4092

Shi Wenlong, Yang Haifeng, Du Xiaofeng, Gao Yanfei, Liu Rui, Tu Xiang, 2022. Paleo-Drainage Restoration and Prediction of Sedimentary Coupling Response in the Southern Bohai Sea. Earth Science, 47(11): 4075-4092. doi: 10.3799/dqkx.2022.022

Citation:

Shi Wenlong, Yang Haifeng, Du Xiaofeng, Gao Yanfei, Liu Rui, Tu Xiang, 2022. Paleo-Drainage Restoration and Prediction of Sedimentary Coupling Response in the Southern Bohai Sea. Earth Science, 47(11): 4075-4092. doi: 10.3799/dqkx.2022.022

Citation:

Shi Wenlong, Yang Haifeng, Du Xiaofeng, Gao Yanfei, Liu Rui, Tu Xiang, 2022. Paleo-Drainage Restoration and Prediction of Sedimentary Coupling Response in the Southern Bohai Sea. Earth Science, 47(11): 4075-4092. doi: 10.3799/dqkx.2022.022

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Paleo-Drainage Restoration and Prediction of Sedimentary Coupling Response in the Southern Bohai Sea

doi: 10.3799/dqkx.2022.022

CNOOC Tianjin Branch, Tianjin 300452, China

Received Date: 2022-01-15
Available Online: 2022-12-07
Publish Date: 2022-11-25

Abstract

Abstract

The modern drainage systems of Jargalant Nuruu and Turgen-Kharkhiraa mountain systems in Inner Mongolia and the paleo-drainage systems of Chengbei low uplift and Bonan low uplift in Bohai Bay basin were picked up by Global Mapper and ArcGIS software, combining the boundary conditions, fracture style and parent lithology, it is considered that water systems are diverse under the combined styles of three elements. Boundary conditions influence the degree of convergence, with low convergence degree of water system in steep slope, and high degree of convergence in slow slope belt. The fracture pattern affects the direction of the water system, in which the boundary fracture intersects the water system vertically, and the oblique crossing fracture develops in the same direction as the water system. Igneous rock has various water system styles, whereas carbonate stratigraphic water system is mainly subparallel, and metamorphic rock formation has dendritic water system. On the whole, there are five styles of single parallel, feather, pectinate, subparallel and dendritic water systems developed. Combining modern source-to-sink system with ancient source-to-sink system of Bohai Bay basin, it shows that different drainage patterns correspond to different sedimentations, including (1) the source system of slow slope/stable slope-boundary fracture-igneous rock/metamorphic rock primary develop firstly water system-dendritic water system, that deposition comprises slope fan and braided river delta, that fan body is large and independent with sand-rich type; (2) slow slope/stable slope-parallel fracture-carbonate rock/igneous rock develop secondary water system-subparallel water system, the sediment comprises alluvial fan and fan dalta, that fan body is small and independent with mud-rich type. The ancient and modern analogy and verification effectively facilitate the prediction of high-quality sedimentary bodies in the underground sedimentary area by accurately picking up the distribution and development characteristics of the water system in the source area, which plays an important role in promoting the coupling of source-to-sink system elements and the exploration and prediction of underground large-scale reservoirs.
- Bohai Bay basin,
- source-to-sink system,
- paleo-drainage pattern,
- provenance system,
- geomorphological-sedimentary response,
- sedimentology

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References(61)

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