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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Chaotic dynamics and fractals in magmatic interaction processes: a different approach to the interpretation of mafic microgranular enclaves
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Chaotic dynamics and fractals in magmatic interaction processes: a different approach to the interpretation of mafic microgranular enclaves

机译:岩浆相互作用过程中的混沌动力学和分形:解释镁铁质微颗粒飞地的另一种方法

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Fractals have been used for describing a wide range of natural processes. However, applications of fractal geometry to the study of magma mingling/mixing processes is almost completely lacking, in spite of the fact that such an approach could give new insights into the nature of magmatic interactions. Fractal analyses of two geochemically linked groups of mafic microgranular enclaves (MME) from the Sithonia Plutonic Complex (Northern Greece) have been performed. Because of the difficulties involved in using contours of enclaves to estimate their fractal dimensions, a different approach is used in this paper. Fractal dimension is estimated using distribution maps of chemical elements inside enclaves. The results obtained indicate that a clear correlation between fractal dimensions of enclaves and geochemical evidences of interaction exists and hence the two groups of enclaves reflect different degrees of interaction. From a dynamical point of view, stretching and folding processes between two magmas with different rheologies are considered representative of magmatic interaction. This dynamic system can easily generate chaotic patterns recognized by the presence of fractal structures. The contemporaneous occurrence of well-mixed regions together with poorly-mixed regions in the same system is thought to be similar to the host/enclave system found in many granitoid plutons. In particular, MME are believed to represent islands of partially-mixed mafic fluid subjected to different degrees of interaction with the host granitoid, whereas host rocks are believed to represent mixed regions where the mixing process acted more efficiently producing almost completely hybrids. It is shown that fractal geometry and chaotic dynamics can be considered suitable techniques in studying complex petrological phenomena and they can represent helpful methods in the development of petrogenetic models.
机译:分形已被用于描述各种自然过程。然而,尽管这种方法可以对岩浆相互作用的性质提供新的见解,但几乎完全缺乏分形几何学在岩浆混合/混合过程研究中的应用。对来自Sithonia Plutonic Complex(希腊北部)的镁铁质微细颗粒飞地(MME)的两个地球化学联系的组进行了分形分析。由于使用飞地的轮廓来估计其分形维数存在困难,因此本文采用了另一种方法。分形维数是使用飞地内部化学元素的分布图估算的。获得的结果表明,飞地的分形维数与相互作用的地球化学证据之间存在明显的相关性,因此两组飞地反映了不同程度的相互作用。从动力学的观点来看,两个具有不同流变性的岩浆之间的拉伸和折叠过程被认为是岩浆相互作用的代表。这个动态系统可以很容易地产生分形结构所识别的混沌模式。人们认为,在同一系统中同时发生混合区域以及混合不良区域的情况与在许多类花岗岩体中发现的宿主/飞地系统相似。特别地,据信MME代表了部分混合的铁镁质流体的孤岛,这些岛状流体与主体花岗岩之间有不同程度的相互作用,而主体岩石被认为代表了混合区域,在该区域混合过程更有效地产生了几乎完全的杂种。研究表明,分形几何学和混沌动力学可以被认为是研究复杂岩石学现象的合适技术,并且它们可以代表开发成岩模型的有用方法。

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