| Qingdao Institute of marine geology, China Geological Survey | Host |
| Citation: |
WANG Wenjuan, ZHANG Yinguo, CHEN Jianwen, YANG Yanqiu. Sequence stratigraphy and sedimentary evolution in the Lower Cretaceous of the Eastern Depression in the North Yellow Sea Basin[J]. Marine Geology & Quaternary Geology, 2024, 44(3): 125-135. doi: 10.16562/j.cnki.0256-1492.2023100701
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Sequence stratigraphy and sedimentary evolution in the Lower Cretaceous of the Eastern Depression in the North Yellow Sea Basin
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Abstract
The Lower Cretaceous of the Eastern Depression in the North Yellow Sea Basin is a favorable reservoir for hydrocarbon exploration. However, scarce studies on its fine stratigraphic delineation and sedimentary evolution have restricted the deep understanding of the prospect of hydrocarbon exploration in the eastern depression. Through the core observation, logging and recording analyses, and well-seismic calibration in the eastern depression, it is concluded that the Lower Cretaceous mainly developed 3 third-order sequences, K1SQ1, K1SQ2, and K1SQ3 in bottom-up order. Only 2 third-order sequences, K1SQ1 and K1SQ2, are visible in the drilling, and the descending half-circle of the K1SQ2 sequence is always incomplete, with only the ascending half-cycle of the sequence remaining. The K1SQ1 was in the period of faulting extension, and the vertical lithological sequence exhibited a complete depositional cycle with progradation-retrogradation. In the early stage, there were fluvial phases which developed at mainly the basin margins, the fan-delta phases were in the southern rift zone of the basin, and the braided river-delta phase was in the northern slow-slope zone. Due to the uprising of the lake level, mudstone-dominated lake deposits were developed in the middle and late stages. In the advanced stage, small-scale braided river delta deposits developed in the northern slow-slope zone. The K1SQ2 was in the period of stabilized rupture, which inherited the depositional characteristics of the K1SQ1 period and contracted slightly. The K1SQ3 was in the period of faulting abortion, which was characterized by the development of a large area of fluvial phase deposits.
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References
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WANG Wenjuan, ZHANG Yinguo, CHEN Jianwen, YANG Yanqiu. Sequence stratigraphy and sedimentary evolution in the Lower Cretaceous of the Eastern Depression in the North Yellow Sea Basin[J]. Marine Geology & Quaternary Geology, 2024, 44(3): 125-135. doi: 10.16562/j.cnki.0256-1492.2023100701
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Figure 1.
Geographic location and tectonic units of the Eastern Dpression in the North Yellow Sea Basin[15]
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Figure 2.
Comprehensive stratigraphic column of the Lower Cretaceous sedimentary strata in the East Depression
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Figure 3.
Seismic and drilling calibration for the sequence stratigraphic
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Figure 4.
Lithology and electrical characteristics of the SB1 sequence boundary in Well C (left) and the characteristics of the paleoweathering crust (right)
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Figure 5.
Lithology and electrical characteristics of the SB1 sequence boundary in Well B (left) and the characteristics of the seismic reflected waves (right)
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Figure 6.
Lithologic and electrical characteristics of the SB2 in Well A
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Figure 7.
Characterization of seismic reflected waves of the SB4 sequences interface
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Figure 8.
Lithologic and electrical characteristics of the SB4 in Well D
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Figure 9.
Divisions and comparisons in sequence stratigraphy among 3 wells
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Figure 10.
Indicators of sedimentary facies in the Eastern Depressions of the North Yellow Sea
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Figure 11.
Sedimentary phase distribution in the K1SQ1-K1SQ3 period
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Figure 12.
The third-order sequences and sedimentary filling patterns in the early cretaceous