| 潍坊涌泉庄膨润土、沸石岩、珍珠岩矿床矿层结构及其成因 |
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| 引用本文： | 李艳双,王玉玲.潍坊涌泉庄膨润土、沸石岩、珍珠岩矿床矿层结构及其成因[J].山东国土资源,1995(2). |
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| 作者姓名： | 李艳双 王玉玲 |
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| 作者单位： | 山东省化学矿地质勘探队，山东省地矿局第一地质队 |
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| 摘 要： | 本文阐述了涌泉庄火山－沉积型膨润土、沸石岩、珍珠岩三位一体矿床的矿层内部结构，将划分为Ａ，Ｂ，Ｃ，Ｄ，Ｅ五种类型。提出了矿床的形成是成矿原岩在外界条件作用下连续去硅的过程，对三矿的共生在成因方面得到了一致的解释。
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THE DEPOSIT STRUCTURES OF WEIFANGYONGQUANZHUANG BENTONTE , ZEOLITE AND PERLITE DEPOSIT AND ITS ORIGIN |
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| Li Yanshuang and Wang Yuling.THE DEPOSIT STRUCTURES OF WEIFANGYONGQUANZHUANG BENTONTE , ZEOLITE AND PERLITE DEPOSIT AND ITS ORIGIN[J].Land and Resources in SHANDONG Province,1995(2). |
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| Authors: | Li Yanshuang and Wang Yuling |
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| Abstract: | The paper elucidates the inner structures of the ore beds in the volcano sedimentarybentonite, Zeolite and perlite three combined in one deposit near Weifang Yongquanzhuangvillage and classifies them into five types of A,B,C,Dand E. It is proposed that the formation ofthe deposit was the result of continuous desilicification of ore forming original rocks under theaction of exogenic forces. For the association of three kinds of deposits a consistent genesisexplanation is given. |
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