Orbital cycle recognition and sequence stratigraphic division of the Lower Carboniferous Dawuba Formation shales in Southwest Guizhou

WANG Jiawei; JIN Siding; WEI Xiangfeng; HAO Jingyu; CHEN Yicai; LI Luyan; MA Chao

doi:10.19509/j.cnki.dzkq.tb20230546

Volume 44 Issue 4

Aug. 2025

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Article Navigation > Bulletin of Geological Science and Technology > 2025 > 44(4): 288-303

WANG Jiawei，JIN Siding，WEI Xiangfeng，et al. Orbital cycle recognition and sequence stratigraphic division of the Lower Carboniferous Dawuba Formation shales in Southwest Guizhou[J]. Bulletin of Geological Science and Technology，2025，44（4）：288-303 doi: 10.19509/j.cnki.dzkq.tb20230546

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Orbital cycle recognition and sequence stratigraphic division of the Lower Carboniferous Dawuba Formation shales in Southwest Guizhou

doi: 10.19509/j.cnki.dzkq.tb20230546

WANG Jiawei^{1a, 1b
,},
JIN Siding^{1a, 1b
,
,},
WEI Xiangfeng²,
HAO Jingyu²,
CHEN Yicai^{1a, 1b},
LI Luyan^{1a, 1b},
MA Chao^{1b, 1c}

1a .
College of Energy, Chengdu University of Technology
1b .
National Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology
1c .
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China, Chengdu University of Technology
2 .
SINOPEC Exploration Company, Chengdu 610041, China

More Information

Author Bio:
E-mail：1091924996@qq.com
Corresponding author: E-mail：jinsiding@cdut.edu.cn
Received Date: 26 Sep 2023
Accepted Date: 18 Jan 2024
Rev Recd Date: 24 Oct 2023

Available Online: 26 Feb 2024

Abstract

Abstract

<p>The Lower Carboniferous Dawuba Formation in Southwest Guizhou hosts a shale sequence with significant exploration potential. Current disagreements regarding its sequence division scheme and developmental mechanisms have somewhat hindered the understanding of the spatial distribution patterns of this high-quality shale.</p></sec><sec><title>Objective
Therefore, this study focuses on the Lower Carboniferous Dawuba Formation shale (interval 1457–2466 m) from the Well Qian Shui Di-1 in Southwest Guizhou.
Methods
Utilizing the natural gamma ray (GR) log as a proxy indicator, methods including time series analysis, INPEFA (integrated noise-enhanced population evolutionary frequency analysis), and wavelet analysis were applied to conduct cyclostratigraphic and sequence stratigraphic investigations. The aim is to achieve a "quantitative" division of the sequence stratigraphy for this shale unit from an astronomical forcing perspective.
Results
The results demonstrate that the Dawuba Formation shale records clear astronomical periodic signals. COCO (correlation coefficient) analysis estimates an optimal average sedimentation rate of 16.4 cm/ka, corresponding to a sediment thickness of 66.42 m for the 405 ka long eccentricity cycle. Spectral analysis and astronomical tuning were performed on segmented GR data from the Well Qian Shui Di-1 (upper segment: 1457-1932 m; lower segment: 1932-2466 m). The optimal sedimentation rates for the upper and lower segments are 16.5 cm/ka and 11.2 cm/ka, respectively. The entire Dawuba Formation recorded 19 long eccentricity cycles, enabling the establishment of a "floating" astronomical time scale, which estimates a total duration of approximately 7.86 Ma for the formation. Furthermore, relative sea-level change curves were reconstructed using sedimentary noise modeling (DYNOT and ρ1 methods).Building upon the temporal framework established by cyclostratigraphy, and integrating relative sea-level extrema, INPEFA, and wavelet analysis results, six third-order sequence boundaries were identified, dividing the formation into five third-order sequences. The development of these third-order sequences is interpreted to be controlled by a stable approximately 1.2 Ma obliquity amplitude modulation cycle.
Conclusion
By applying cyclostratigraphy to the sequence division of the Dawuba Formation shale, this study explores the relationship between astronomical orbital parameters and relative sea-level change at different temporal scales, achieving the division of both third-order and fourth-order sequences. This methodology enables potential high-resolution (10000-year scale) chronostratigraphic correlation of marine shales. It provides a refined temporal framework for predicting intervals of high-quality source rock development within shale sequences, thereby offering crucial theoretical guidance for shale oil and gas exploration.
- cyclostratigraphy,
- time series analysis,
- sequence stratigraphy,
- sea-level change,
- obliquity amplitude modulation,
- shale,
- Southwest Guizhou

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References(87)

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Orbital cycle recognition and sequence stratigraphic division of the Lower Carboniferous Dawuba Formation shales in Southwest Guizhou

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Orbital cycle recognition and sequence stratigraphic division of the Lower Carboniferous Dawuba Formation shales in Southwest Guizhou

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