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物探与化探  1986, Vol. 10 Issue (4): 274-281    
  论文 本期目录 | 过刊浏览 | 高级检索 |
应用重力资料划分地壳类型的一种方法
曹洛华
湖北省地质科学研究所
A NEW METHOD FOR DIVISTON OF THE EARTH'SCRUST BY USING GRAVTY DATA
Cao Luohua
Institute of Geological Sciences, Bureau of Geology andMineral Resources of Hubei Prcvince
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摘要 

在与矿产有关的深部参数中,地壳基性度可用以反映地壳的组分或平均化学成份的差异。本文提出应用重力资料计算地壳视基性度的方法,并对几个有影响的参量做了一些讨论;又根据地壳视基性度提出划分地壳类型和计算壳内界面深度的方法,介绍了在鄂东南地区的应用结果。

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关键词 定义方程导出单位一贯单位制    
Abstract

Of various parameters of depths related to ore resources,the basicity mightreflect the differences in components or average chemical composition of theearth's crust. Amethod for calculating apparent basicity of the crust by usinggravity data is proposed in this paper with a discussion on some relativelydecisive parameters. Atechnique for dividing the crust and calculating thedepths of interfaces within the crust is also presented on the basis of apparentbasicity together with a description of its application in southeastern Hubei.

Key wordsdefinite equation    derived unit    coherent system of units
     出版日期: 1986-08-24
引用本文:   
曹洛华. 应用重力资料划分地壳类型的一种方法[J]. 物探与化探, 1986, 10(4): 274-281.
Cao Luohua. A NEW METHOD FOR DIVISTON OF THE EARTH'SCRUST BY USING GRAVTY DATA. Geophysical and Geochemical Exploration, 1986, 10(4): 274-281.
链接本文:  
https://www.wutanyuhuatan.com/CN/      或      https://www.wutanyuhuatan.com/CN/Y1986/V10/I4/274

[1] 程家印编译:1982年,区城物探与地质找矿,物探与化探译丛,1-2期。
[2] 刘元龙,王谦身,1977年,用压缩质面法反演重力资料以估计地壳构造,地球物理学报,20卷1期

[1] 袁方. 磁化率、电极化率、电位移等物理量的单位及其换算[J]. 物探与化探, 2008, 32(4): 448-450.
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