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辽东裂谷硼铁矿床地质及成矿作用
引用本文:夏学惠,阎 飞,赵玉海,常文宗.辽东裂谷硼铁矿床地质及成矿作用[J].矿床地质,2006,25(1):83-88.
作者姓名:夏学惠  阎 飞  赵玉海  常文宗
作者单位:中化地质矿山总局地质研究院,河北,涿州,072754
摘    要:辽东硼铁矿床是一处类型独特的超大型矿床。文章对该矿床的地质特征、矿石物质组成、矿床稀土元素和稳定同位素特征及矿化时代进行了研究。研究表明,该矿床的成矿作用主要表现为海底热水沉积成矿,区域变质混合岩化作用对矿床进行了强烈的叠加改造,使硼铁进一步富集而形成工业矿床。

关 键 词:地质学  硼铁矿床  地质特征  成矿作用  辽东裂谷
文章编号:0258-7106(2006)01-0083-06
收稿时间:2005-06-09
修稿时间:2005-06-092005-09-28

Geological features and ore_forming process of uranium_bearing vonsenite deposit in Liaodong rift, eastern Liaoning Province, China
XIA XueHui,YAN Fei,ZHAO YuHai,CHANG WenZong.Geological features and ore_forming process of uranium_bearing vonsenite deposit in Liaodong rift, eastern Liaoning Province, China[J].Mineral Deposits,2006,25(1):83-88.
Authors:XIA XueHui  YAN Fei  ZHAO YuHai  CHANG WenZong
Abstract:The uranium-bearing vonsenite deposit in Liaodong (eastern Liaoning) is a unique and superlarge deposit. In this paper, the authors studied the ore composition, ore-forming epoch, REE characteristics and stable isotopes of this deposit based on a detailed investigation of geological features of this type of deposits. The results indicate that submarine hot water deposition is the main ore-forming process of the uranium-bearing vonsenite deposit, and that the economic deposit was formed on the basis of further enrichment of boron and iron through the superposition and transformation by regional metamorphism and migmatization.
Keywords:geology  vonsenite deposit  geological features  ore-forming process  Liaodong rift
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