黄骅坳陷上古生界深部煤层气主控因素及成藏模式

李宏军; 陈长伟; 董晓伟; 秦晨烊; 甘华军; 卢碧娴; 付一鸣

doi:10.3799/dqkx.2026.239

Volume 51 Issue 7

Jul. 2026

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Li Hongjun, Chen Changwei, Dong Xiaowei, Qin Chenyang, Gan Huajun, Lu Bixian, Fu Yiming, 2026. Main Controlling Factors and Accumulation Models of Upper Paleozoic Coalbed Methane in Huanghua Depression. Earth Science, 51(7): 2514-2527. doi: 10.3799/dqkx.2026.239

Citation:

Li Hongjun, Chen Changwei, Dong Xiaowei, Qin Chenyang, Gan Huajun, Lu Bixian, Fu Yiming, 2026. Main Controlling Factors and Accumulation Models of Upper Paleozoic Coalbed Methane in Huanghua Depression. Earth Science, 51(7): 2514-2527. doi: 10.3799/dqkx.2026.239

Citation:

Li Hongjun, Chen Changwei, Dong Xiaowei, Qin Chenyang, Gan Huajun, Lu Bixian, Fu Yiming, 2026. Main Controlling Factors and Accumulation Models of Upper Paleozoic Coalbed Methane in Huanghua Depression. Earth Science, 51(7): 2514-2527. doi: 10.3799/dqkx.2026.239

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Main Controlling Factors and Accumulation Models of Upper Paleozoic Coalbed Methane in Huanghua Depression

doi: 10.3799/dqkx.2026.239

Li Hongjun^{1
,
,},
Chen Changwei¹,
Dong Xiaowei¹,
Qin Chenyang^{2, 3
,
,
,},
Gan Huajun^{2, 3},
Lu Bixian^{2, 3},
Fu Yiming^{2, 3}

1.
Research Institute of Exploration and Development, PetroChina Dagang Oilfield Company, Tianjin 300280, China
2.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences (Wuhan), Wuhan 430074, China
3.
Inner Mongolia Research Institute, China University of Geosciences (Wuhan), Ordos 017000, China

Received Date: 2025-07-05
Publish Date: 2026-07-25

Abstract

Abstract

The Huanghua Depression is characterized by complex structural units. The Upper Paleozoic coal seams show marked spatial variations in burial depth, thermal maturity, and preservation conditions, and the enrichment patterns and accumulation types of coalbed methane remain unclear. This study integrated coal-thickness distribution, coal petrographic and coal-quality characteristics, plane distribution of vitrinite reflectance (R_o), burial-thermal evolution histories of typical wells, tectonic evolution, and borehole evidence of magmatic rocks to analyze the controls of sedimentation, tectonic deep burial, and magmatism on coalbed methane accumulation. The coal thickness and lateral continuity of the Taiyuan Formation are generally better than those of the Shanxi Formation, and the Wangguantun-Wumaying and Kongdian-Chenghai areas are the main coal-accumulation zones. Tectonic deep burial resulted in regional high maturity and differentiation of preservation conditions; multi-stage tectonic inversion caused reservoir adjustment; and magmatic thermal events led to abnormally high maturity in shallow-burial areas or structural highs, and could further modify deeply buried coal measures. Coalbed methane enrichment in the study area is jointly controlled by burial heating, tectonic adjustment, and magmatic thermal modification. Four accumulation models are identified: shallow-burial magmatic model, tectonic deep-burial model, multi-stage tectonic inversion model, and deep-burial magmatic model. This study provides a theoretical basis for favorable area selection and exploration potential evaluation of Upper Paleozoic CBM in the Huanghua Depression.
- Huanghua Depression,
- Upper Paleozoic,
- coalbed methane,
- main controlling factor,
- accumulation model,
- tectonic evolution,
- magmatic thermal modification

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References(60)

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Main Controlling Factors and Accumulation Models of Upper Paleozoic Coalbed Methane in Huanghua Depression

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