Citation: | ZHANG Dong, SUN Zhilei, ZHANG Xilin, WU Nengyou, LUO Di, GENG Wei, XU Cuiling, CAO Hong. Research progress of multi-azimuth acquisition and imaging technology of wide-tow multi-sources dual-sensor streamer[J]. Marine Geology & Quaternary Geology, 2022, 42(4): 194-206. doi: 10.16562/j.cnki.0256-1492.2021110801 |
Wide-tow multi-sources dual-sensor streamer multi-azimuth acquisition and imaging technology has been successfully introduced into commercial seismic exploration projects. It improves the resolution of near-bottom strata and deep seismic images. This paper details this novel acquisition and imaging technique. This paper summarizes its application effect in the identification of near-seabed strata and deep target geological bodies in the North Sea, offshore Malaysia, the Barents Sea and other sea areas. The acquisition solution innovatively combines dual-sensor streamers, wide-tow multi-sources, and different length streamer arrangements with the new multi-azimuth acquisition. The Complete wavefield imaging combines reflection tomography, full waveform inversion (FWI), and separated wavefield imaging (SWIM). Its advantages mainly include: (1) Significantly weaken the influence of rough sea surface reflection and broaden the seismic frequency band. (2) Improve the signal-to-noise ratio, spatial sampling density, acquisition efficiency and velocity model accuracy. (3) Realize near offset uniform coverage and cost-effective multi-azimuth lighting. It can perform high-resolution imaging of near-seabed formations and deep geological targets, especially in shallow marine environmental conditions. It provides a cost-effective solution for imaging geological bodies at different depths.
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Source towing and streamer configuration[1]
CMP line coverage[1]
Complementary CMP line coverage for a wide-tow source acquisition[1]
Schematic illustration of the pressure wavefields [33]
A high density 16×56.25 m streamer spread[29]
The GeoStreamer X multi-azimuth acquisition configurations[14]
FWI velocity updates overlaid depth migration stack[29]
FWI sensitivity kernel at 9 Hz for long offset refractions over sand-injectites [14]
Velocity model overlaid seismic profile[44]
FWI velocity model[29]
Schematic diagram of wave field recorded by dual-sensor[16]
Seismic profile of crossline in shallow water of Malaysia [46]
Complete wavefield imaging workflow[21]
Acquisition scheme[5]
Applications in the Barents Sea[14]
Imaging comparison of single azimuth and multi-azimuth acquisition schemes[14]