Asser区块Karloff-Oxford群礁碳酸盐组地震响应及波群特征

Zeng Zhongyu, Zheng xuyao, Hong qiyu
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引用次数: 1

摘要

基于阿姆河右岸Asser地块上侏罗统Karloff-Oxford组的地质特征和电性特征,建立了生物礁复杂地质模型,并采用波动方程正演模拟方法研究了碳酸盐岩地层的地震响应。该区礁杂岩的地震反应特征为丘状反射和透镜反射特征。地震波在礁群边缘常出现叠上和绕射地震反射现象,反射波顶部存在上弯现象。礁体顶部反射波为槽式弱反射,波幅弱,波前不连续。礁群内反射波无组织或微弱,在振幅、频率和相位上与围岩的连续性差异较大。此外,与双翼构造相比,我们发现内部礁群反射波所暗示的厚度更大。上述特征与井上礁复合体地震剖面特征一致。因此,我们利用礁群的正演模拟结果,建立了礁群地震特征识别模式。
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Seismic Response and Wave Group Characteristics of Reef Carbonate Formation of Karloff-Oxford Group in Asser Block
In this article, we built a reef complex geological model, which is based on the geological characteristics and electric characteristics on the upper Jurassic Karloff-Oxford Formation of Asser Block at the Right Bank of the Amu River, and studied seismic response of carbonate formation by the wave equation forward modeling. Seismic response characteristics of reef complex in the area are the mound-shaped and lenticular reflections characteristics. Seismic wave in the edges of the reef complex often appear onlap and diffraction seismic reflection phenomenon, and there is upper bend phenomenon on the top of the reflection wave. The reflection wave on the top of the reef complex is trough weak reflection, with weak amplitude and discontinuous wave-front. The internal reflection wave in reef complex are unorganized or weakly, and there is a big difference in continuity between it and that of the surrounding rock on the amplitude, frequency and phase. Moreover, compared with formations of two wings, we found out that the thickness suggested by the reflection waves in the internal reef complex is bigger. The characteristics mentioned above are consistent with seismic section characteristics of reef complex over well. So that, we built a characteristics to recognize pattern of seismic of reef complex by using forward modeling results of a reef complex.
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