Combined interpolation and primary estimation
US-2015362608-A1 · Dec 17, 2015 · US
US9810801B2 · US · B2
| Field | Value |
|---|---|
| Publication number | US-9810801-B2 |
| Application number | US-201514963929-A |
| Country | US |
| Kind code | B2 |
| Filing date | Dec 9, 2015 |
| Priority date | Apr 7, 2015 |
| Publication date | Nov 7, 2017 |
| Grant date | Nov 7, 2017 |
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Provided is a method for swell effect and mis-tie correction in high-resolution marine seismic data using multi-beam echo sounder data, and more particularly, a method for swell effect and mis-tie correction in high-resolution marine seismic data using multi-beam echo sounder data capable of acquiring the high-resolution marine seismic data having the swell effect and the mis-tie effectively corrected by using the multi-beam echo sounder data including water depth data of a sea-bottom having high precision.
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What is claimed is: 1. A method for correcting a swell effect and a mis-tie at the intersection point of marine seismic data using multi-beam echo sounder data measured by a multi-beam sounder, the method comprising: receiving the multi-beam echo sounder data; extracting water depth values corresponding to positions having latitude and longitude coordinate points same as shot points at the marine seismic data in the multi-beam echo sounder data; correcting the swell effect and the mis-tie at the coordinate points of the marine seismic data by reflecting the water depth values; and deriving the marine seismic data at which the swell effect and the mis-tie are corrected by performing the extracting and the correcting on all coordinate points at the marine seismic data. 2. The method of claim 1 , wherein the correcting the swell effect and the mis-tie comprises: calculating a first sea-bottom two-way travel time to which the water depth value is reflected by converting the water depth value into a two-way travel time using a vertical sound velocity of a sea water measured upon acquiring the multi-beam echo sounder data; extracting a second sea-bottom two-way travel time corresponding to a coordinate point in the marine seismic data; and correcting the swell effect and the mis-tie at the coordinate point of the marine seismic data by comparing the first sea-bottom two-way travel time with the second sea-bottom two-way travel time. 3. The method of claim 2 , wherein the correcting the swell effect and the mis-tie at the coordinate point of the marine seismic data by comparing the first sea-bottom two-way travel time with the second sea-bottom two-way travel time comprises: calculating a difference value between the first sea-bottom two-way travel time to which the water depth value is reflected and the second sea-bottom two-way travel time; and correcting the swell effect and the mis-tie by applying the difference value to the entire two-way travel time at the coordinate point of the marine seismic data. 4. A non-transitory computer readable recording medium storing a program for implementing a method for correcting a swell effect and a mis-tie at the intersection point of marine seismic data using multi-beam echo sounder data measured by a multi-beam sounder, the method comprising: receiving the multi-beam echo sounder data; extracting water depth values corresponding to positions having latitude and longitude coordinate points same as shot points at the marine seismic data in the multi-beam echo sounder data: correcting the swell effect and the mis-tie at the coordinate points of the marine seismic data by reflecting the water depth values; and deriving the marine seismic data at which the swell effect and the mis-tie are corrected by performing the extracting and the correcting on all coordinate points at the marine seismic data. 5. The non-transitory computer readable recording medium of claim 4 , wherein the correcting the swell effect and the mis-tie comprises: calculating a first sea-bottom two-way travel time to which the water depth value is reflected by converting the water depth value into a two-way travel time using a vertical sound velocity of a sea water measured upon acquiring the multi-beam echo sounder data; extracting a second sea-bottom two-way travel time corresponding to a coordinate point in the marine seismic data; and correcting the swell effect and the mis-tie at the coordinate point of the marine seismic data by comparing the first sea-bottom two-way travel time with the second sea-bottom two-way travel time. 6. The non-transitory computer readable recording medium of claim 5 , wherein the correcting the swell effect and the mis-tie at the coordinate point of the marine seismic data by comparing the first sea-bottom two-way travel time with the second sea-bottom two-way travel time comprises: calculating a difference value between the first sea-bottom two-way travel time to which the water depth value is reflected and the second sea-bottom two-way travel time; and correcting the swell effect and the mis-tie by applying the difference value to the entire two-way travel time at the coordinate point of the marine seismic data.
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