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反演地壳磁化强度等效源法的模型验证及实际资料试算
引用本文:王京,张昌达.反演地壳磁化强度等效源法的模型验证及实际资料试算[J].物探与化探,1993,17(3):201-208.
作者姓名:王京  张昌达
作者单位:地矿部航空物探遥感中心 北京100083 (王京),中国地质大学 武汉430074(张昌达)
摘    要:等效源法曾被广泛应用于卫星磁异常解释,而本文是将等效源法引用到航空△T磁场的解释中,用其研究区域地质构造。根据等效源法的理论,推导出球坐标系下球棱柱体的△T磁场公式,采用线性反演的方法进行模型验证,同时将该方法用于秦巴地区航空△T磁异常的试算,得到了一些有意义的结论。利用该方法可由所求得的磁场强度来得到居里深度分布。

关 键 词:航空△T激场解释方法  等效源法
收稿时间:1991-10-31

MODEL TEST OF THE EQUIVALENT SOURCE METHOD FOR INVERSION OF MAGNETIZATION INTENSITY OFTHE CRUST AND TENTATIVE CALCULATION OF AVAILABLE DATA
Wang Jing.MODEL TEST OF THE EQUIVALENT SOURCE METHOD FOR INVERSION OF MAGNETIZATION INTENSITY OFTHE CRUST AND TENTATIVE CALCULATION OF AVAILABLE DATA[J].Geophysical and Geochemical Exploration,1993,17(3):201-208.
Authors:Wang Jing
Institution:1. Aerogeophysical Remote Sensing Center, Ministry of Geology and MineralResources, Beijing 100083;
2. China university of Geosciences, Wuhan 430074
Abstract:Abstract The equivalent &ource method has been extensively used ia the interpretation of satel- lite magnetic anomalies. Ia this paper, however, the equivalent source method is introduced into the interpretation of the aarbmagnetic AT field to investigate regional tectonics. Based on the theory of the equivalent source method, we deduced a formula for Ar magnetic field of the lower spherical prism of the spherical coordinate system, and made model test using the linear inversion method. This method was used to make tentative calculation of aeromagnetic T ano- malies in Qinlins-Bashan area and, as a result, reached some valuable conclusions. With this method, the Curie depth distribution can be obtained from the calculated magnetic field inten- sity.
Keywords:Key words interpretation method of aeromagnetic T  field  equivalent source method    
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