节点文献
广东连平大顶铁矿床地质特征及成因探讨
Geological Characteristics and Genesis of the Dading Iron Deposit in Guangdong Lianping
【摘要】 本文以连平大顶铁矿床为研究对象,对该矿床成矿地质特征进行了综合分析研究,并对其成因进行了探讨,研究认为大顶铁矿床的形成经历了十分复杂的地质作用,它经历了同生沉积或火山-喷流沉积、热变质改造和花岗岩浆的热液叠加作用,最后形成了现在的矿床。
【Abstract】 This paper lays emphasis on the geological characteristics and genesis of the Dading iron deposit in Lingping,Guangdong province.It is concluded that the Dading iron deposit through the formation of a very complex geological processes,with the synsedimentary or volcanic-exhalative stage,thermal maturation transformation stage and magmatic hydrothermal overprinting in the deposit,then in the end form the current deposit.
【关键词】 铁矿床;
地质特征;
矽卡岩;
成因探讨;
连平大顶;
【Key words】 iron deposit; geological characteristics; skarn; genesis; Lianping Dading;
【Key words】 iron deposit; geological characteristics; skarn; genesis; Lianping Dading;
- 【文献出处】 甘肃冶金 ,Gansu Metallurgy , 编辑部邮箱 ,2009年01期
- 【分类号】P618.31
- 【被引频次】8
- 【下载频次】200