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Influence of near surface structure on multi-wave exploration at the mountain front of South Junggar Basin |
Zhi-Guo CHENG1, Ting-Ting HU1, Ling-Yun WEI1, Hai-Yang GUO2 |
1. GRI,Exploration and Production Research Academe,Xinjiang Oilfield Company,Urumqi 830013,China 2. Seismic Exploration Research Center,East Geophysics Company(Xinan),Chendu 610213,China |
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Abstract In Junggar basin,near surface structure is an obvious factor influencing seismic data.2D 3C seismic line data were collected recently at Gaoquan anticline of the mountain front area.Nevertheless,S/N of PS-wave section was obviously lower than P-wave section at the east end of 2D line.To verify and analyze near surface structure's influence on multi-wave 3C seismic data,the authors built forward model by using its near surface structure and well-logging data so as to get modeling shots with real acquisition geometry.By analysis of modeling results and near surface structure investigation,it is found that the thickness of low velocity layer increases and Xiyu conglomerates are developed at the east end of 2D line because of Kuitun River's sedimentation,which is the main reason of energy and S/N reduction of multi-wave seismic data.It is also proved that PS wave is more easily influenced by near surface structure's attenuation than P wave.
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Received: 28 September 2018
Published: 15 August 2019
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Survey's structure and position map
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名称 | 参数 | 名称 | 参数 | 观测方式 | 宽线 | 观测系统 | 2L2S2000R | 道距/m | 10 | 激发点距/m | 40 | 接收道数/道 | 2000 | 最小炮检距/m | 5 | 纵向排列方式 | 9995-5-5-9995 | 最大炮检距/m | 9995 | 纵向覆盖次数 | 250 | 接收线距/m | 40 | 横向覆盖次数 | 4 | 激发线距/m | 40 | 覆盖次数 | 1000 | 采样间隔/ms | 2 | 记录长度/s | 10 | | |
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Geometry parameters tab of 2D line A201719
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PP(a) and PS(b) pre-stack migration section of A201719
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Survey's satellite map
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Near surface structure model of A201719
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Typical PP and PS reflection amplitude versus offset
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地质层位 | 地震层位 | 纵波速度/(m·s-1) | 密度/(g·cm-3) | 新近系沙湾组 | N1s | 3180 | 2.5 | 古近系紫泥泉子组 | E1-2z | 3500 | 2.55 | 白垩系清水河组 | K1q | 2.60 | 3900 | 侏罗系头屯河组 | J2t | 2.55 | 4150 | 侏罗系西山窑组 | J2x | 2.50 | 3150 | 侏罗系西山窑组之下 | | 2.62 | 4000 |
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Seismic forward model information tab
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P-wave Velocity section of forward model(a),PP wave stack section(b) and PS wave stack section(c)
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Time-frequency analysis results of different time window of one shot at eastern part of A201719
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