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湘中中奥陶世优质锰矿地球化学特征
引用本文:吴永胜,曹景良.湘中中奥陶世优质锰矿地球化学特征[J].湖南地质,2003,22(2):101-106.
作者姓名:吴永胜  曹景良
作者单位:中南地勘局长沙地质调查所,中南地勘局长沙地质调查所 湖南 长沙 410011,湖南 长沙 410011
摘    要:简要介绍了朗中地区中奥陶世锰矿含矿岩系、矿体形态、矿石等—般特征,重点总结了该类型锰矿的常量元素、微量元素、稳定同位素及稀土元素、有机地球化学特征.提出:①朗中地区中奥陶世锰矿是低磷、低铁、高碱度优质锰矿石;②成矿的物质来源为多源,既有陆源,也有深部热液来源;⑦锰沉积成矿过程中,有机质起了极其重要作用.

关 键 词:中奥陶世  锰矿床  湖南  稳定同位素  稀土元素  有机地球化学  锰沉积  有机质  常量元素  微量元素

GEOCHEMISTRY TRAITS OF HIGH GRADE Mn-ORES OF MIDDLE ORDOVICIAN EPOCH IN CENTRAL HUNAN
WU Yong-sheng,CAO Jing-liang.GEOCHEMISTRY TRAITS OF HIGH GRADE Mn-ORES OF MIDDLE ORDOVICIAN EPOCH IN CENTRAL HUNAN[J].Hunan Geology,2003,22(2):101-106.
Authors:WU Yong-sheng  CAO Jing-liang
Abstract:The common traits of the ores, ore body conformation and ore-bearing rock series of Middle Ordovician Epoch in central Hunan were briefly introduced; the traits of organic geochemistry, RE, stable isotopes, microelements and macro-elements of the kind of Mn-ores were summarized emphatically. That a: The Mn-deposits of Middle Ordovician Epoch in central Hunan were high grade Mn-ores with low-P, low-Fe and high basicity; b: The metallogenic materials came from the terrigenous and deep hydrothermal solution; c: Organic matter played an important role in metallogenic period of Mn sediment, were put forward.
Keywords:Geochemistry traits  High grade Mn-ores  Middle Ordovician Epoch  Central Hunan  
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