前言传统的储量计算方法(平行断面法、地质块段法等)是把地质体划分成若干部分,每部分以简单的几何形体来表示,对于品位、厚度等仅取平均值,作为常数来处理,并没有考虑它们在空间上的变异性。实际上矿体并不是规则的几何形体,品位、厚度等在空间均是变化的变量,而且这种变化具有一定的随机性。而克里金法、能算出各块段真实品位的估计值的一种地质统计学方法。这种方法即考虑到地质变量的随机性,同时又 Preface Traditional reserves calculation method (parallel section method, geological block method, etc.) is divided into several parts of the geological body, each part of a simple geometric representation, for the grade, thickness, etc. only average, as a constant to deal with , Did not consider their spatial variability. In fact, the ore body is not a regular geometric body, grade, thickness and so on are variables in the space of change, and this change has a certain degree of randomness. The Klinkin method, a geostatistical method that can calculate the true value of each block, This method takes into account the randomness of geological variables, at the same time