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在磁法勘探中,确定岩(矿)石磁化强度矢量,是一项极为重要的工作.由于观测条件的限制,在野外不可能直接测得磁化强度的各个分量,而是依靠在选定地点采集定向标本,在室内进行测量并作统计分析,求出磁化强度矢量.室内测定岩(矿)石标本的仪器种类和方法很多.测定精度各不相同,通常测量误差在n～30%之间.因为测量标本所得出的统计平均值是该子样中所有标本的平均数,所以从误差理论来说,测量误差的影响因取平均会有很大的降低.可是事实并非如此.在解磁法勘探正、反演问题时,经常发现合适的磁化强度与标本测定统计的磁化强度相
It is an extremely important task to determine the magnetization intensity of rock (rock) in magnetic exploration.Due to the limitation of observation conditions, it is impossible to directly measure the components of magnetization in the field, Acquisition of directional specimens, indoor measurements and statistical analysis, to find the magnetization vector.Indoor rock (ore) stone specimens of many types of instruments and methods.Determination of precision vary, usually measuring error between n ~ 30% Since the statistical average of the measured specimens is the average of all the specimens in the subsample, the effect of the measurement error on average is greatly reduced from the error theory, but this is not the case. Law exploration is positive, inversion problems, often found that the appropriate magnetization and specimen measured the magnetization phase