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柳钢罗城排刘哲宜同志对平果一带第四纪铁矿成因及分布规律进行研究,发表了第一篇科学报告,现摘要介绍如下。 她首先介绍了平果一带的地质概况,然后阐述铁矿分布规律与地区构造的关系。她认为有两个现象: 1.构造中部感兴背斜及果化背斜中C_1,及C_2h地层出露的喀斯特灰岩盆地中铁转石较多而向新地层P_1c、p_1m铁转石减少,平果背斜中之转石相对其它两箱状背斜为少,感兴背斜由中部向东部滚石也渐减少。
Comrade Liu Zheyi, Liucheng Row of Liu Gang, studied the causes and distribution of Quaternary iron deposits in Pingguo area and published the first scientific report. The summary is as follows. She first introduced the geological overview of the Pingguo area and then explained the relationship between iron ore distribution and regional structure. She thinks there are two phenomena: 1. In the karst limestone basins of the central horizons and fruit anticlines C_5 and C_2h, there are more stones transferred from the China Railway to the P_1c and p_1m of new strata, Pinggu anticline of the stone relative to the other two box-shaped anticlines less, feel the anticlines from the middle to the east of Rolling also gradually reduced.