首页|期刊导航|河北地质大学学报|用爱因斯坦的质能方程分析地球内部圈层构造的形成原理

用爱因斯坦的质能方程分析地球内部圈层构造的形成原理OACHSSCD

Analysis of the Formation Principle of Earth's Internal Stratigraphic Structure Using Einstein's Mass-Energy Equation

中文摘要英文摘要

受实验工具耐受高温高压条件的限制,高温高压实验仅能较为合理地研究地壳及上地幔顶部的物质成分特征.而基于物理及物理化学的基本原理进行推演,是探究地幔与地核成分更为可信的方法.作者运用质能转换方程、牛顿重力原理和普朗克尺度这三个公认的基本原理,系统分析了地球内部圈层的形成过程,以及各圈层物质的运动状态与成分特征.初步研究认为,在高温高压的超临界状态下,即便在地球深部,也可能存在与成矿作用相关的流体相物质,这可为成岩成矿作用的研究提供有益启示.

The author argues that high-temperature and high-pressure experiments,constrained by experimental instruments' limitations in withstanding extreme conditions,can only provide reasonable insights into the compositional characteristics of the crust and upper mantle.In contrast,deriving conclusions from fundamental principles of physics and physical chemistry offers a more reliable approach for investigating mantle and core composition.Based on three established principles-the mass-energy transformation equation,Newton's law of gravitation,and Planck's scale-the author systematically analyzes the formation processes of Earth's internal spheres,along with the motion states and compositional features of materials within each layer.Preliminary research suggests that fluid-phase materials related to mineralization processes may exist even in deep Earth regions under supercritical conditions of extreme temperatures and pressures,providing valuable insights for studies on diagenesis and mineralization processes.

张建珍

河北地质大学,河北 石家庄 052161

天文与地球科学

爱因斯坦地球圈层物理化学普朗克尺度学科交叉

Einsteinearth's spheresphysical chemistryPlanck scaleinterdisciplinary studies

《河北地质大学学报》 2026 (4)

46-55,10

10.13937/j.cnki.hbdzdxxb.2026.04.005

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