Mesonorm标准矿物计算法:一个有用的岩石学工具
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1.中国地质大学(北京)地球科学与资源学院;2.中国地质大学北京地球科学与资源学院

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中国地质调查局地质调查项目(D1912)


Mesonorm Calculation Method: A Useful Tool for Petrological Studies
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1.School of Earth Sciences and Resources,China University of Geosciences;2.School of Earth Sciences and Resources, China University of Geosciences, Beijing

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    摘要:

    Mesonorm是适用于火成岩和高级变质岩的由全岩化学成分计算标准矿物含量的方法。与得到广泛应用的CIPW标准矿物计算方法相比,Mesonorm方法通过引入黑云母(Bi)标准分子,减少了计算结果中钾长石(Or)标准分子的含量。对于大多数常见的火成岩和中高级变质岩,Mesonorm方法提供了更接近于实际的钾长石含量估计值。本文简要介绍Mesonorm的计算步骤,并给出几个研究实例以显示Mesonorm作为标准矿物计算方法的优点。对于含云母类矿物的常见侵入岩的分类命名而言,其Mesonorm标准矿物在QAP和Q’-ANOR图解的投影点可以给出正确的结果,而CIPW标准矿物的投影点经常错判。基于化学-矿物学准则厘定的5大类花岗质岩石组合,其Mesonorm标准矿物在Q’-ANOR图解的投影图式(pattern)各不相同。这一事实表明Mesonorm标准矿物的Q’-ANOR图解投影可用于识别未知花岗岩套的化学-矿物学类型。根据Mesonorm标准矿物估算的中国东部地区中高级正变质岩的密度值与其全岩SiO2含量之间存在良好的相关性,即:SiO2 (wt%) = -69.069 × ρ + 259.741(密度ρ的单位:103kg/m3)。由此估算出中国东部下地壳的SiO2含量低于53 wt%,化学成分属于基性。我们认为,Mesonorm标准矿物比CIPW标准矿物更适合于常见火成岩和中高级变质岩的研究。然而,目前缺少计算Mesonorm的软件,尚需更多的编程工作来解决这个问题。

    Abstract:

    Mesonorm is a norm calculation scheme from whole-rock chemical analyses of igneous or high grade metamorphic rocks. Compared with the widely used CIPW norm scheme, a major improvement of the mesonorm scheme is introducing the biotite (Bi) norm in its calculation procedure. Thus, the mesonorm scheme produces less content of K-feldspar (Or) norm and more content of quartz (Q) norm for most igneous and high grade metamorphic rocks. Consequently, the mesonorm provides a more realistic estimation of the K-feldspar content in the rocks. In this paper, the procedure of mesonorm calculation is presented briefly, and several case studies are provided to validate the advantages of the mesonorm as a tool for normative calculations. For the naming and classification of the mica contained plutonic rocks, the norms by mesonorm calculations project into the right places of the QAP and the Q’-ANOR diagrams, while the CIPW norms performs badly in the cases. The mesonorm projections of five categories of granitoids, which are defined by the chemical-mineralogical criteria, illustrates distinguishable patterns in the Q’-ANOR diagram among the five categories. This finding suggests that the mesonorm projected Q’-ANOR plot is a potential scheme to identify the chemical-mineralogical categories of granitoid suites and discriminate their tectonic environment. The bulk rock densities of the intermediate- and high-grade ortho-metamorphic rocks in eastern China, which are derived from the rock-forming mineral portions by mesonorm calculations, demonstrate a good correlation with their bulk SiO2 contents, which is SiO2 (wt%) = -69.069 × ρ + 259.741 (the unit of density ρ is 103kg/m3). Thus the bulk SiO2 content of the lower crust of eastern China is estimated to be less than 53 wt%, and implies a basic composition in chemistry. In summary, we argue that the mesonorm provides more suitable norms than the CIPW norms for common igneous and high-grade metamorphic rocks. However, the public softwares for mesonorm calculation are still lacking, and more programming works are needed.

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  • 收稿日期:2025-07-30
  • 最后修改日期:2025-09-20
  • 录用日期:2025-10-22
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