花岗岩深部风化作用研究

Katsunori Tanaka
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引用次数: 0

摘要

目前还没有找到合适的方法来研究这种被称为马萨的深风化花岗岩的质地、结构和矿物组成。本文报道了笔者对崩解花岗岩和风化花岗岩进行了系统的研究。其方法是分析离断层的距离与颗粒直径的关系,并对颗粒大小分布、视比重、地震测深、电法勘探、地形起伏量等进行累积曲线分析。笔者所研究的地区几乎覆盖了六野山、兵库县、道吾县、爱媛县、八岛县、香川县、佐治县、爱知县等全部地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on the Deepseated Weathering of Granites
No suitable method has yet been found for the study on the texture, the structure and the mineral composition of the deep weathered granites, which has been called the Masa. In this paper, it is reported that the writer has made the systematic study of the disintegrated and the weathered granites. Its method is the analysis of the relationship between the distance from the fault and the diameter of the particles, and also the analysis of the cumulative curve for the size distribution, the apparent specific gravity, the seismic sounding, the elect1' ic prospecting, the relief quantity. The area reseached by the writer covered nearly over the whole area of Rokko mountains, Hyogo Pref., Dogo Dist., Ehime Pref., Yashima, Kagawa Pref., Sanage Dist., Aichi Pref. and the other regions.
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