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    准噶尔盆地东道海子凹陷中、深层地震波组特征及地质意义

    Characteristics and geological significance of seismic wave groups from medium-deep strata in Dongdaohaizi Sag, Junggar Basin

    • 摘要: 准噶尔盆地东道海子凹陷勘探潜力大,勘探程度低。利用目标区内已钻深井的钻录井资料和新采集的二维、三维地震数据制作合成地震记录并进行层位标定,精细刻画东道海子凹陷中、深层地震波组特征,明确区内勘探潜力。在测井曲线特征分析和合成地震记录标定的基础上,识别出中、深层二叠系顶底及内幕清晰的4个反射界面:T0,T1,T2,T3。总结了凹陷内中、深层地层主要地震波组特征:T0为二叠系与石炭系之间的界面,也是盆地内可进行区域对比的关键标志层;T1为二叠系将军庙组与烃源岩发育段平地泉组之间的界面;T2为平地泉组与上乌尔禾组之间的界面;T3为三叠系与二叠系之间的界面,也是晚二叠世与三叠纪之间的区域不整合面的地层响应。地震剖面精细解释成果揭示了东道海子凹陷中、深层地震波组特征及地质意义,主要目的层上乌尔禾组(即T2与T3之间)由4 ~ 6个波峰−波谷组成,连续性中等,可见较强同相轴能量的横向减弱或频率的变化,反映湖侵背景下的岩性砂体特征。西北凹槽区上乌尔禾组的“上超”波组特征反映该区存在较大物源体系,是下一步风险勘探的有利区。

       

      Abstract: The Dongdaohaizi Sag in the Junggar Basin has a great exploration potential, but it has been less explored. In this paper, selected deep wells and newly acquired 2D and 3D seismic data within the Dongdaohaizi Sag were used to produce synthetic seismic records and perform horizon calibration, so as to identify the characteristics of seismic wave groups from medium–deep strata in the sag and clarify the exploration potential of the study area. On the basis of log characterization and synthetic seismic record calibration, four clear reflection interfaces, T0, T1, T2, and T3, were identified at the top and bottom and in the interior of the medium–deep Permian system. The characteristics of main seismic wave groups from the medium–deep strata in the sag were summarized. Specifically, T0 is the interface between the Permian and the Carboniferous, and it is the key marker bed for regional correlation in the basin. T1 is the interface between the Permian Jiangjunmiao Formation and the Pingdiquan Formation with source rocks developed. T2 is the interface between the Pingdiquan Formation and the Upper Wuerhe Formation. T3 is the interface between the Triassic and the Permian, and it represents the response of the regional unconformity between the Late Permian and the Triassic. Based on the detailed interpretation of seismic profiles, the characteristics and geological significance of seismic wave groups from the medium–deep strata in the Dongdaohaizi Sag were revealed. It is found that the seismic profile of the Upper Wuerhe Formation (between T2 and T3), the key target horizon, is composed of 4–6 wave peaks and troughs, with moderate continuity, as well as the transverse attenuation of the strong event energy or frequency change, which reflects the characteristics of lithologic sand bodies deposited under the background of lake transgression. The "onlapped" wave group characteristics of the Upper Wuerhe Formation in the northwestern part of the sag reflect the existence of a large provenance system, making this area a favorable target for future risk exploration.

       

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