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首页> 外文期刊>Natural resources research >Complexity and Productivity Differentiation Models of Metallogenic Indicator Elements in Rocks and Supergene Media Around Daijiazhuang Pb-Zn Deposit in Dangchang County, Gansu Province
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Complexity and Productivity Differentiation Models of Metallogenic Indicator Elements in Rocks and Supergene Media Around Daijiazhuang Pb-Zn Deposit in Dangchang County, Gansu Province

机译:甘肃省党昌县戴家庄铅锌矿床周围岩石和表生介质中成矿指示元素的复杂性和生产力区分模型

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摘要

With the help of complexity indices, we quantitatively studied multifractals, frequency distributions, and linear and nonlinear characteristics of geochemical data for exploration of the Daijiazhuang Pb-Zn deposit. Furthermore, we derived productivity differentiation models of elements from thermodynamics and self-organized criticality of metallogenic systems. With respect to frequency distributions and multifractals, only Zn in rocks and most elements except Sb in secondary media, which had been derived mainly from weathering and alluviation, exhibit nonlinear distributions. The relations of productivity to concentrations of metallogenic elements and paragenic elements in rocks and those of elements strongly leached in secondary media can be seen as linear addition of exponential functions with a characteristic weak chaos. The relations of associated elements such as Mo, Sb, and Hg in rocks and other elements in secondary media can be expressed as an exponential function, and the relations of one-phase self-organized geological or metallogenic processes can be represented by a power function, each representing secondary chaos or strong chaos. For secondary media, exploration data of most elements should be processed using nonlinear mathematical methods or should be transformed to linear distributions before processing using linear mathematical methods.
机译:借助复杂性指标,我们定量研究了地球化学数据的多重分形,频率分布以及线性和非线性特征,用于勘探戴家庄铅锌矿床。此外,我们从热力学和成矿系统的自组织临界性导出了元素的生产率差异模型。关于频率分布和多重分形,仅岩石中的Zn和次生介质中除Sb以外的大多数元素(主要来自风化和冲积)显示出非线性分布。生产率与岩石中成矿元素和副生元素的浓度以及在次级介质中强烈浸出的元素的浓度之间的关系可以看作是具有特征性弱混沌的指数函数的线性加法。岩石中的Mo,Sb和Hg等相关元素与二次介质中其他元素的关系可以表示为指数函数,一相自组织地质或成矿过程的关系可以由幂函数表示,每个代表次要混乱或强烈混乱。对于次要介质,大多数元素的勘探数据应使用非线性数学方法进行处理,或者应在使用线性数学方法进行处理之前转换为线性分布。

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