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Multivariate analysis, mass balance techniques, and statistical tests as tools in igneous petrology: application to the sierra de las cruces volcanic range (mexican volcanic belt)

机译:多变量分析,质量平衡技术和统计测试作为火成岩学的工具:在拉克鲁斯塞拉山脉火山岩范围(墨西哥火山带)中的应用

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摘要

Magmatic processes have usually been identified and evaluated using qualitative or semiquantitative geochemical or isotopic tools based on a restricted number of variables. However, a more complete and quantitative view could be reached applying multivariate analysis, mass balance techniques, and statistical tests. As an example, in this work a statistical and quantitative scheme is appliedudto analyze the geochemical features for the Sierra de las Cruces (SC) volcanic range (Mexican Volcanic Belt). In this locality, the volcanic activity (3.7 to 0.5 Ma) was dominantly dacitic, but the presence of spheroidal andesitic enclaves and/or diverse disequilibrium features in majority of lavas confirms the operation of magma mixing/mingling. New discriminant-function-based multidimensional diagrams were used to discriminate tectonic setting. Statistical tests of discordancy and significance were appliedudto evaluate the influence of the subducting Cocos plate, which seems to be rather negligible for the SC magmas in relation to several major and trace elements. A cluster analysis followingWard’s linkage rule was carried out to classify the SC volcanic rocks geochemical groups. Finally, two mass-balance schemes were applied for the quantitative evaluation of the proportion of the end member components (dacitic and andesitic magmas) in the comingled lavas (binary mixtures).
机译:通常基于有限数量的变量,使用定性或半定量地球化学或同位素工具来识别和评估岩浆作用过程。但是,使用多变量分析,质量平衡技术和统计测试,可以获得更完整和定量的观点。例如,在这项工作中,采用了一种统计和定量方案来分析塞拉德拉克鲁斯山脉(SC)火山范围(墨西哥火山带)的地球化学特征。在该地区,火山活动(3.7至0.5 Ma)主要为达吉奇岩,但大多数熔岩中球形安第斯飞地和/或各种不平衡特征的存在证实了岩浆混合/混合的作用。新的基于判别函数的多维图被用来区分构造背景。应用不一致和显着性的统计检验来评估俯冲的Cocos板块的影响,这对于SC岩浆相对于几个主要和微量元素而言似乎可以忽略不计。根据Ward的关联规则进行了聚类分析,以对SC火山岩地球化学类别进行分类。最后,采用两种质量平衡方案定量评估了混合熔岩(二元混合物)中端部组分(胶质岩和安第斯岩浆)的比例。

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    Velasco Tapia Fernando;

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  • 年度 2014
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  • 正文语种 en
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