Enhancement of seismic data gathered by floating ice acquisition : Application of local kinematic attributes. / Khaidukov, V. G.; Neklyudov, D. A.; Silvestrov, I. Y. et al.
In: SEG Technical Program Expanded Abstracts, Vol. 35, 2016, p. 4654-4658.Research output: Contribution to journal › Conference article › peer-review
}
TY - JOUR
T1 - Enhancement of seismic data gathered by floating ice acquisition
T2 - SEG International Exposition and 86th Annual Meeting, SEG 2016
AU - Khaidukov, V. G.
AU - Neklyudov, D. A.
AU - Silvestrov, I. Y.
AU - Protasov, M. I.
AU - Tcheverda, V. A.
AU - Reshetova, G. V.
AU - Landa, E.
PY - 2016
Y1 - 2016
N2 - The presence of large areas covered by shallow waters, like swamps, rivers, lakes and so on, troubles seismic exploration in the Russian Far North in summer. The winter seems to be much more appropriate time to implement seismic acquisitions for reasonable cost but with acceptable quality of the data. The same is true for transition zones. Really, in winter there is possible, at least technically, use floating ice and apply the developed technology for onshore seismic study. But in winter there is another complicating factor - intensive seismic noise generated by sources placed onto ice covering shallow waters. It is well known that this noise is connected with flexural waves propagating along the ice. These waves are much slower than surface waves, which are well studied for onshore acquisitions and, hence, seem to be easy avoided by the modern versions of f-k filters. Unfortunately, straightforward application of this type of noise suppression fails. To understand the matter, the representative series of numerical experiments are conducted which prove that the main impact to noise is multiple conversions of flexural waves to the body ones and vice versa. Ways to reduce this noise by special processing procedures are proposed and discussed.
AB - The presence of large areas covered by shallow waters, like swamps, rivers, lakes and so on, troubles seismic exploration in the Russian Far North in summer. The winter seems to be much more appropriate time to implement seismic acquisitions for reasonable cost but with acceptable quality of the data. The same is true for transition zones. Really, in winter there is possible, at least technically, use floating ice and apply the developed technology for onshore seismic study. But in winter there is another complicating factor - intensive seismic noise generated by sources placed onto ice covering shallow waters. It is well known that this noise is connected with flexural waves propagating along the ice. These waves are much slower than surface waves, which are well studied for onshore acquisitions and, hence, seem to be easy avoided by the modern versions of f-k filters. Unfortunately, straightforward application of this type of noise suppression fails. To understand the matter, the representative series of numerical experiments are conducted which prove that the main impact to noise is multiple conversions of flexural waves to the body ones and vice versa. Ways to reduce this noise by special processing procedures are proposed and discussed.
UR - http://www.scopus.com/inward/record.url?scp=85019062582&partnerID=8YFLogxK
U2 - 10.1190/segam2016-13809298.1
DO - 10.1190/segam2016-13809298.1
M3 - Conference article
AN - SCOPUS:85019062582
VL - 35
SP - 4654
EP - 4658
JO - SEG Technical Program Expanded Abstracts
JF - SEG Technical Program Expanded Abstracts
SN - 1052-3812
Y2 - 16 October 2011 through 21 October 2011
ER -
ID: 25776497