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The parameter choice and application in correspondence analysis on gravity and magnetic anomalies

机译:重力和磁异常对应分析的参数选择与应用

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In addition to studying the correlation coefficient R and slope B of correspondence analysis method of gravity and magnetic anomalies, this paper pay more attention to the commonly neglected parameter, intercepts A, in order to get the relationship between anomalies and geological bodies. By the experiment of a three dimensional body theories model, we found: (1) the density of spacing of dots and lines did not almost influence the result of calculation. (2) The space of slip windows chosen is fit to 1.4-2 times of model radius. (3) When the gravity and magnetic anomalies are mostly correlated, it is not over 30° that the degree of the surplus magnetizing direction deviating from terrestrial magnetic field direction or the opposite side of the terrestrial magnetic field), when they are somewhat correlated, it is small or be equal to 45°. when they are weakly correlated or not correlated, it is 45°-135°. (4) For a single model research, excluding the condition that the gravity anomalies and magnetic anomalies have different source or abnormal disturbs each other, we thought intercepts was the anomaly that brought from strong surplus magnetic geological body after Poisson window filted waves. We studied the distribute scope of strong magnetic and surplus magnetic in 1:1,000,000 map of Northeast China the positions of deep and large faults and the volcano organization in 1:250,000 map of the mountain regions in Inner Mongolia according to field data processing by this method.
机译:除了研究重力和磁性异常的对应分析方法的相关系数R和斜率B之外,本文还需要更多地关注常用的参数,拦截A,以便获得异常和地质体之间的关系。通过三维体理论模型的实验,我们发现:(1)点和线条间距的密度几乎影响了计算结果。 (2)所选择的滑动窗口的空间适合模型半径的1.4-2次。 (3)当重力和磁异常大多是相关的时,当它们有些相关的情况时,剩余磁化方向偏离陆地磁场方向或相对的侧面的剩余磁化方向的程度不超过30°。它很小或等于45°。当它们弱或不相关时,它为45°-135°。 (4)对于单一的模型研究,不包括引力异常和磁性异常具有不同的源或异常的条件,我们认为截止者是从泊松窗中剥离波浪后从强剩余磁性地质体带来的异常。我们研究了磁力和盈余磁力的分布范围:1,000,000地图,在中国东北地区的境地和火山组织的位置1:250,000地图在内蒙古的山地地图,根据此方法的现场数据处理。

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