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作 者:李晶晶[1] Li Jingjing(Chengdu University of Technology,Chengdu 610059,China)
机构地区:[1]成都理工大学,成都610059
出 处:《黑龙江科学》2024年第2期38-40,共3页Heilongjiang Science
摘 要:地球的内部结构与化学组成对于理解其构造、演化及地质活动非常关键。为深入探讨地球内部物质的化学成分及其与地球构造的关系,从多个地质钻探点收集了大量的岩石样本并进行详细的化学分析,使用统计图表对数据进行可视化。结果显示,地壳主要由硅酸盐矿物组成,富含硅和氧,地幔和核则含有较多的铁、镁及其他重元素,化学成分与地质活动,如地震和火山喷发之间存在密切关系。数据分析显示,地震活动的频率与地区的硅含量之间存在正相关性,这对理解地球内部物质的化学成分及其构造与地质活动至关重要。未来,需要在更深的地方进行钻探研究,结合多学科知识更全面地探索地球内部。The internal structure and chemical composition of the earth are critical to understanding its structure,evolution,and geological activity.In order to explore the chemical composition of the interior materials,and their relationship with the structure of the earth,the study collects a large number of rock samples from multiple geological drilling sites,conducts detailed chemical analysis,and visualizes the data with statistical charts.The results show that the crust is mainly composed of silicate minerals.It is rich in silicon and oxygen.The mantle and core contains more iron,magnesium and other heavy elements.There is close relationship between chemical composition and geological activities,such as earthquakes and volcanic eruptions.The results of data analysis show that there is positive correlation between the frequency of seismic activity and the silicon content of the region,which is crucial to understanding the chemical composition of materials in the interior earth and its structure and geological activity.In the future,it is necessary to conduct drilling studies in depth,and comprehensively explore the interior of the earth with the combination of multidisciplinary knowledge.
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