Seismic study of gas hydrate BSR in the Okinawa Trough

TANG Yong; JIN Xiang-long; FANG Yin-xia; SUN Peng; LI Xin

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TANG Yong, JIN Xiang-long, FANG Yin-xia, SUN Peng, LI Xin. Seismic study of gas hydrate BSR in the Okinawa Trough[J]. Haiyang Xuebao, 2003, 25(4): 59-66.

Citation:

TANG Yong, JIN Xiang-long, FANG Yin-xia, SUN Peng, LI Xin. Seismic study of gas hydrate BSR in the Okinawa Trough[J]. Haiyang Xuebao, 2003, 25(4): 59-66.

TANG Yong, JIN Xiang-long, FANG Yin-xia, SUN Peng, LI Xin. Seismic study of gas hydrate BSR in the Okinawa Trough[J]. Haiyang Xuebao, 2003, 25(4): 59-66.

Citation:

TANG Yong, JIN Xiang-long, FANG Yin-xia, SUN Peng, LI Xin. Seismic study of gas hydrate BSR in the Okinawa Trough[J]. Haiyang Xuebao, 2003, 25(4): 59-66.

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Seismic study of gas hydrate BSR in the Okinawa Trough

Key Laboratory of Submarine Geosciences of State Oceanic Administration, Hangzhou 310012, China;Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China

Received Date: 2001-09-12
Rev Recd Date: 2002-09-05

Abstract

Abstract

According to the analysis of multichannel seismic reflection data,the BSRs are found in the southern and central areas of Okinawa Trough.The analyses of seismic attributions of amplitude,velocity and AVO explain that the BSRs are generated by the gas hydrate.And it is found that gas hydrate is closely related to fault in the Okinawa Trough.
- BSR,
- gas hydrate,
- AVO,
- seismic processing

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References(12)

References

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