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在论述欧拉反褶积基础理论与方法的基础上,以我国某海域航空重力资料为例,对该海域内地质异常体(侵入岩、断鼻构造)及断裂构造等进行了欧拉反褶积反演计算,获得了场源深度等信息,确定了场源位置及边界,并与航空布格重力异常、垂向导数、上延、水平梯度模、剩余异常以及重磁联合反演结果等资料相互验证,取得了很好的应用效果.基于该地区的反演效果,证明欧拉反褶积法可应用于航空重力勘探中,可为其他航空重力勘探区计算场源位置及深度信息提供可靠并且准确的研究方法,从而达到辅助航空重力勘探测量的效果.
Based on the discussion of the basic theory and method of Euler deconvolution, taking the gravity data of aero-region in China as an example, the Eulerian detritus is carried out on the geological anomalies (intrusive rocks, broken nose structures) and fault structures in this area. Inverse inversion calculation and field source depth information were obtained, and the locations and boundaries of field sources were determined. The results were compared with those of Bouguer gravity anomalies, vertical derivatives, up-delay, horizontal gradient modes, residual anomalies, The results show that the Euler deconvolution method can be applied in the gravity exploration of the aviation and can provide the information for calculating the location and depth of field sources in other aerial gravity exploration areas Reliable and accurate research methods, so as to achieve the effect of auxiliary aviation gravity survey.