Application of Hilbert-Huang transform method in fine illustrating shallow marine sediment system

Lu Yintao; Cao Xiaochu; Ran Weimin; Luan Xiwu; Xu Xiaoyong; Li Dong; Yang Taotao; Shao Dali; Wei Xinyuan

doi:10.12284/hyxb2021061

Volume 43 Issue 5

May 2021

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Lu Yintao，Cao Xiaochu，Ran Weimin, et al. Application of Hilbert-Huang transform method in fine illustrating shallow marine sediment system[J]. Haiyang Xuebao，2021, 43(5)：100–109 doi: 10.12284/hyxb2021061

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Application of Hilbert-Huang transform method in fine illustrating shallow marine sediment system

doi: 10.12284/hyxb2021061

Lu Yintao^1
,,
Cao Xiaochu¹,
Ran Weimin^{2, 3
,
,},
Luan Xiwu^{2, 3},
Xu Xiaoyong¹,
Li Dong¹,
Yang Taotao¹,
Shao Dali¹,
Wei Xinyuan^{3, 4}

1.
China Petroleum Hangzhou Institute of Geology, Hangzhou 310023, China
2.
Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, China
3.
Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266237, China
4.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China

Received Date: 2020-03-12
Rev Recd Date: 2020-04-15

Available Online: 2021-03-24

Publish Date: 2021-07-06

Abstract

Abstract

The complex subaqueous channel system of shallow and transition facies is developed in the Pliocene-Pleistocene strata at the conjunction area of Malay Basin and West Natuna Basin, and can not be characterized in detail by conventional seismic data. By applying Hilbert-Huang transform to post-stack seismic data, the high frequency components of seismic data were extracted, the resolution of seismic data was improved, and the interaction characteristics of thin layer sand and mudstone and small sedimentary bodies were identified effectively. Through the instantaneous attribute extraction of the high frequency component, the plane distribution characteristics of the underwater branch channels in the target interval are defined. Compared with conventional post-stack seismic attributes, the instantaneous attributes extracted from post-stack seismic data after Hilbert-Huang transform show more detailed features of sedimentary system. And it provides high-resolution seismic data for the study of spatio-temporal evolution of underwater branch channels, such as internal structure, development period and cutting relationship.
- Hilbert-Huang transform,
- instantaneous attributes,
- marine-continental transitional sediment,
- multi-period river channel evolution

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References(33)

References

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