Abstract
Few seismic exploration work was carried out in Tibetan Plateau due to the characteristics of alpine hypoxia and harsh environmental protection needs. Complex near surface geological conditions, especially the signal shielding and static correction of permafrost make the quality of seismic data is not ideal, the signal to noise ratio (SNR) is low, and deep target horizon imaging is difficult. These data cannot provide high quality information for oil and gas geological survey and structural sedimentary research in the area. To solve the issue of seismic exploration in Tibetan Plateau, this test used low frequency vibroseis wide-line and high-density acquisition scheme. In view of the actual situation of the study area, the terrain, the source and the different observation system were simulated, and the processing technique was adopted to improve the quality of seismic data. Low-frequency components with a minimum of 1.5Hz of vibroseis ensure the deep geological target imaging quality in the area, the seismic profile wave group is clear, and the SNR is relatively high, which can meet the needs of oil and gas exploration. Seismic data can provide the support for the development of oil and gas survey in the Tibet plateau.
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We are grateful to Wang Jianmin, an expert of Daqing Oilfield Exploration and Development Research Institute, for his guidance and help in the process of writing this paper.
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This work was supported by Nation key R&D program (No. 2016YFC060110305) and Geological and mineral investigation and evaluation special project (No. DD20160160 and No. DD20160181).
Tian Yu-Kun Ph.D. graduated from China University of Petroleum (Beijing) in 2013. He is currently working in the Oil and Gas Survey of China Geological Survey. His main research interests are seismic data processing and reservoir inversion.
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Tian, YK., Kang, Hx., Cao, J. et al. Experiments on excitation and data processing of low-frequency vibroseis in permafrost area of the tibetan plateau. Appl. Geophys. 17, 834–843 (2020). https://doi.org/10.1007/s11770-018-0714-5
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DOI: https://doi.org/10.1007/s11770-018-0714-5