壳幔岩石矿物物性参数整合

    Physical property parameters of rocks and minerals in the crust and the mantle

    • 摘要: 为理解壳-幔物质密度、速度结构的地质意义,在历时数年的地质-地球物理综合解释工作成果的基础上,整合壳-幔岩石矿物物性参数资料,供地学工作者加深对中国大陆深层区域构造格架的认识。一般来说,随深度增加地壳、地幔和外核岩石矿物密度和速度有正相关的变化规律。从曲线图、柱状图、表格、构造层、岩石矿物多个角度阐述壳-幔岩石矿物物性参数的变化规律,提供综合解释地球内部物质组成的地质-地球物理基础资料。

       

      Abstract: To understand the crust-mantle material density and velocity structure geological significance, the crust-mantle physical property parameters of data are intergrated based on the years of geological and geophysical comprehensive interpretation work. Generally speaking, along with the increased depth of the earth's crust, mantle and outer core density and velocity are positive correlation. From various perspectives (graphs, bar charts, forms, structural layer, rock mineral) of crust-mantle physical parameters change rule, geological and geophysical comprehensive interpretation key basic data of matter in the interior of the earth are provided in the research.

       

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