日本地球惑星科学連合2018年大会

講演情報

[EJ] 口頭発表

セッション記号 S (固体地球科学) » S-SS 地震学

[S-SS10] 地震波伝播:理論と応用

2018年5月23日(水) 13:45 〜 15:15 A10 (東京ベイ幕張ホール)

コンビーナ:西田 究(東京大学地震研究所)、白石 和也(海洋研究開発機構)、新部 貴夫((株)地球科学総合研究所、共同)、澤崎 郁(防災科学技術研究所)、座長:武村 俊介(防災科研)、矢部 優(海洋研究開発機構)

15:00 〜 15:15

[SSS10-06] 陸上低周波データ取得と広帯域データ処理の適用を主体とした地震探査記録品質の改善

*新部 貴夫1村上 文俊1淺川 栄一1阿部 進2佐藤 比呂志3石山 達也3 (1.(株)地球科学総合研究所、2.石油資源開発株式会社、3.東京大学地震研究所)

キーワード:低周波、広帯域

Imaging deep structures using land seismic data acquired in complex terrains of Japan often faces problems since the geology is often complex and target is usually deep volcanic. Recently, acquisition of long-offset high density data using combination of cable and cable-free systems in complex terrain is standardized in domestic land acquisition. First Arrival Travel-Time Tomography is applied to such data to estimate subsurface velocity structure where conventional velocity analysis is difficult because of the above mentioned problems, and recently FWI is applied following tomography to estimate detailed velocity structure.

Low frequency components are known to be effective to FWI and other inversion stability. Also, they are known to be effective to deep imaging and enhancing resolution through reducing side lobes of wavelets. Since around mid-2000s, various techniques has been established to acquire low-frequency in both onshore and offshore environments. Especially, land techniques are important to us since those techniques are capable to Japan onshore environment and the low frequency components are expected to be effective to above mentioned domestic situations.

We have been developed such onshore broad band techniques recently. On source side, conventional linear sweep has problem producing effective low frequency energy because there are some limits in vibrator mechanics and hydraulic. However, the low frequency dwelling non-linear sweeps has been developed around 2008 and we have also developed such sweeps especially suited to our vibrators. On receiver side, conventional 10Hz geophone has problem sensing low frequency because the response of geophone below natural frequency usually reduced. But recently, low frequency sensors such as high sensitivity low frequency geophone and MEMS sensor are commercialized and commonly used in seismic acquisition.

We will show some case study of data acquisition using those techniques. The result is verified by comparing with legacy data. In addition to data acquisition techniques, we have applied some data processing techniques which are not used in legacy data. The processing techniques include combination of noise removal techniques, surface consistent deconvolution, accurate velocity estimation and pre-stack imaging. Also we have applied some broad band techniques such as geophone response correction and spectral whitening using wavelet transform. By combined effect of those recently developed techniques, our result show great improvement compared to legacy data.