Identifying gas hydrate occurrence state by seismic P-wave attenuation in northern South China Sea
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
http://link.springer.com/article/10.1007/s12303-017-0064-y/fulltext.html
Reference22 articles.
1. Biot, M.A., 1962, Mechanics of deformation and acoustic propagation in porous media. Journal of Applied Physics, 33, 1482–1498.
2. Carcione, J.M. and Picotti, S., 2006, P-wave seismic attenuation by slow-wave diffusion: effects of inhomogeneous rock properties. Geophysics, 71, O1–O8.
3. Chand, S. and Minshull, T.A., 2004, The effect of hydrate content on seismic attenuation–a case study from Mallik 2L-38 well data, Mackenzie Delta, Canada. Geophysical Research Letters, 31, L14609. doi:10.1029/2004GL020292
4. Daigle, H. and Dugan, B., 2010, Origin and evolution of fracturehosted methane hydrate deposits. Journal of Geophysical Research, 115, B11103. doi:10.1029/2010JB007492
5. Feng, J., Wang, Y., Li, X., Li, G., Zhang, Y., and Chen, Z., 2015, Production performance of gas hydrate accumulation at the GMGS2-Site 16 of the Pearl River Mouth Basin in the South China Sea. Journal of Natural Gas Science and Engineering, 27, 306–320.
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