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ASSESSMENT METHOD industrial applicability of geological bodies

机译:评估方法地质主体的工业适用性

摘要

1. A method of estimating industrial applicability geological body, comprising: definition mineralogical composition of geologic body; ! building a number of successive ontogenic formation geological body minerals; ! establishing a correlation between the ontogenic next sequential formation geological body minerals and industrial applicability geologic body. ! 2. A method according to claim 1, characterized in that the construction of a number of successive ontogenic formation geological body minerals produced by the relative states of geological age minerals and alternately repeated crystallization of the grain in the unit of one mineral and / or between aggregates of various minerals. ! 3. A method according to claim 1 or 2, characterized in that the construction! ontogenic series of sequential formation of geological body of minerals produced in the descending order of the relative age of the geological conditions of minerals, the mineral is formed on the growth surface, considered to be more ancient than the overgrowing its mineral. ! 4. A method according to claim 1 or 2, characterized in that! the construction of a number of successive ontogenic formation of geological body of minerals produced from the formula: Ab1 Vb1 A2bB2 (A3, B3) Cb1 A4bC2 (A5, C3) V4bS4 (B5, C5) ... Nb1 A6bN2 (A7, N3) V6bN4 (B7, N5) C6bN6 (C7, N7) ..., where! A, B, C, N - state geologic body minerals comprising minerals nucleation, dorastanie minerals transformation grain / crystal grains b unit / unit of crystals, leaching minerals tectonics on minerals, twinning / dedvoynikovanie minerals inclusion the fauna and flora in mineral
机译:1.一种估计工业适用性地质体的方法,包括:定义地质体的矿物学组成; !建立大量连续的成因构造地质体矿物; !建立本体下一个后续形成的地质体矿物与工业适用地质体之间的相关性。 ! 2.根据权利要求1所述的方法,其特征在于,构造由地质年龄矿物的相对状态产生的多个连续的本体形成地质体矿物,以及以一种矿物为单位和/或以各种矿物质的聚集体。 ! 3.根据权利要求1或2所述的方法,其特征在于,所述结构!矿物质的地质序列的本体形成系列是按照矿物质的地质条件的相对年龄的降序排列而产生的,该矿物质在生长表面上形成,被认为比其过度生长的矿物更古老。 ! 4.根据权利要求1或2所述的方法,其特征在于!由以下公式产生的矿物质地质体的多个连续本体形成的构造:Ab1> Vb1> A2bB2>(A3,B3)> Cb1> A4bC2>(A5,C3)> V4bS4>(B5,C5)> ..> Nb1> A6bN2>(A7,N3)> V6bN4>(B7,N5)> C6bN6>(C7,N7)...,哪里! A,B,C,N状态地质体矿物,包括成核矿物,dorastanie矿物转化晶粒/晶粒b单位/晶体,在矿物上浸出矿物构造,孪生/ dedvoynikovanie矿物包括矿物中的动植物群

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