滦平盆地下白垩统西瓜园组震积软沉积变形

郑宁; 宋天锐; 程木伟

doi:10.3799/dqkx.2020.021

Volume 45 Issue 11

Nov. 2020

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Article Navigation > Earth Science > 2020 > 45(11): 4198-4206

Zheng Ning, Song Tianrui, Cheng Muwei, 2020. K1 Xiguayuan Formation Soft-Sediment Deformation Caused by Earthquake in Luanping Basin. Earth Science, 45(11): 4198-4206. doi: 10.3799/dqkx.2020.021

Citation:

Zheng Ning, Song Tianrui, Cheng Muwei, 2020. K₁ Xiguayuan Formation Soft-Sediment Deformation Caused by Earthquake in Luanping Basin. Earth Science, 45(11): 4198-4206. doi: 10.3799/dqkx.2020.021

Zheng Ning, Song Tianrui, Cheng Muwei, 2020. K1 Xiguayuan Formation Soft-Sediment Deformation Caused by Earthquake in Luanping Basin. Earth Science, 45(11): 4198-4206. doi: 10.3799/dqkx.2020.021

Citation:

Zheng Ning, Song Tianrui, Cheng Muwei, 2020. K₁ Xiguayuan Formation Soft-Sediment Deformation Caused by Earthquake in Luanping Basin. Earth Science, 45(11): 4198-4206. doi: 10.3799/dqkx.2020.021

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K₁ Xiguayuan Formation Soft-Sediment Deformation Caused by Earthquake in Luanping Basin

doi: 10.3799/dqkx.2020.021

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Asia-Pacific Department, PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China

Received Date: 2020-02-14
Publish Date: 2020-11-15

Abstract

Abstract

In order to improve the understanding of soft-sediment deformation structures caused by earthquake of the Xiguayuan Formation in Luanping basin, they were studied by the method of combination of both the field investigation with laboratory analysis, and the macroscopic sedimentary system with microscopic soft-sediment deformation structure. In two sections at the angle between the main and secondary basin-controlling faults in the basin, pillow structure, liquefied sand veins, liquefied sand emplacement, liquefied breccias, liquefaction curl deformation, liquefied droplet, flame structure, ball-and-pillow structure, pillow beds, load structure and seismic unconformity plane were developed. Seismites deposited continuously in fan delta front. According to the location of these soft-sediment deformation, their association, continuous development and regional distribution, two successive earthquakes can be identified.
- Luanping basin,
- Xiguayuan Formation,
- soft-sediment deformation,
- earthquake,
- sedimentology

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References(61)

References

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K1 Xiguayuan Formation Soft-Sediment Deformation Caused by Earthquake in Luanping Basin

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K₁ Xiguayuan Formation Soft-Sediment Deformation Caused by Earthquake in Luanping Basin