中文摘要: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。
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.
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基金项目:国家地质大调查项目(编号：1212010331002)
引用文本：
夏学惠，阎 飞，赵玉海，常文宗.2006.辽东裂谷硼铁矿床地质及成矿作用[J].矿床地质,25(1):83~88夏学惠，阎 飞，赵玉海，常文宗.2006.Geological features and ore_forming process of uranium_bearing vonsenite deposit in Liaodong rift, eastern Liaoning Province, China[J].Mineral Deposits25(1):83~88
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