Subsidence History of Northern Qinshui Basin

Kang Liu; You Fei Li; Ai Jun Guo

doi:10.4028/www.scientific.net/AMR.868.62

Paper Titles

Characteristics of Fault and its Controlling to Hydrocarbon Accumulation in the Yumin Area Northern, Songliao Basin
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The Research on the Depositional Systems Types and Characteristics of Sublacustrine Fan Deposits in the Second Member of Dongying Formation, Liaodong Bay
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Deposition Characteristics and Exploration Significances in Shallow-Water Delta Deposits of the First Member of Dongying Formation, Esso3d Area, Liaodong Bay Basin
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The Influence of Tectonic Characteristics on the Accumulation of CBM in H Area
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Subsidence History of Northern Qinshui Basin
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Accumulation Mechanism of Ultro-Low Permeability Sandstone Reservoir, Huaqing Oilfield, Ordas Basin
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Main Controlled Elements for Accumulation of Ultro-Low Permeability Sandstone Oil Reservoir, Zhenjing Oilfield, Ordas Basin
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Petrological Characteristics of Donghe Sandstone Reservoir in HD4 Oil Field
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Mass Change Calculation of the Bauxite in the WZD Area, Northern Guizhou, China
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HomeAdvanced Materials ResearchAdvanced Materials Research Vol. 868Subsidence History of Northern Qinshui Basin

Subsidence History of Northern Qinshui Basin

Abstract:

Based on the data of coalfield drilling and geological information, using the back-stripping technique, the subsidence history of northern Qinshui basin is studied in this paper. The study shows that this area experienced three stages of subsidence and two stages of uplift since Permo-Carboniferous period. It subsided slowly from Late Carboniferous to middle Permian and then subsided rapidly from Late Permian to Triassic period. It uplifted and denuded from Jurassic period to Cretaceous because of Yanshan movement and continued to uplift and denude since Cenozoic because of Himalayan movement and then subsided from Neocene to Quaternary period. The subsidence center mainly migrated from the south to the north since late Paleozoic. The denudation in the east is more than in the west and the largest denudation thickness is over 1000 m.

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Periodical:

Advanced Materials Research (Volume 868)

Pages:

62-65

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.868.62

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Online since:

December 2013

Authors:

Kang Liu*, You Fei Li, Ai Jun Guo

Keywords:

Qinshui Basin, Subsidence Curve, Subsidence History

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