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我国北方农业区尚无工业磷矿床发現,解决这种分布不平衡的問題,巳是一項迫切的任务。本文想将太行山东麓震旦系底部两个磷矿区(下称甲、乙矿区)的主要地貭特征作一介紹,并对其形成条件及找矿远景提出一些浮浅的看法,以引起有关方面的注意。撰写本文时得到地貭队領导和有关同志的鼓励和帮助,在此表示感謝。因所收集实际資料不够充足,作者业务水平不高,不免在文內有謬誤之处,敬請批評指正。
There are no industrial phosphorite deposits in northern China’s agricultural areas yet. To solve this imbalanced distribution problem, it is an urgent task. In this paper, we want to introduce the main characteristics of the two phosphate rock formations at the bottom of the Sinian in the eastern foot of the Taihang Mountains (hereinafter referred to as “A” and “B”), and provide some superficial views on their formation conditions and prospects of prospecting in order to arouse the relevant Aspects of the attention. At the time of writing, I was grateful for the encouragement and help from the leadership of the Diwang team and the comrades concerned. Due to insufficient actual data collected, the author’s business is not high, inevitably there are fallacies in the text, please comment criticism.