东昆仑洪水河铁锰矿床特征及发现意义
Geological Characteristics of the Hongshuihe Iorn-manganese Deposit in Eastern Kunlun Metallogenic Belt and Its Discovery Significance
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摘要: 沉积变质型锰矿是国内外重要的矿床类型,洪水河铁锰矿床是近年来东昆仑地区铁锰矿勘查的重要发现.笔者在对洪水河铁锰矿床成矿地质背景和矿床特征研究基础上,认为矿床产于蓟县系狼牙山组,矿体受地层层位和岩性控制明显,铁锰矿床的形成经历了碎屑沉积、热水沉积、变质作用和表生氧化作用,矿质的沉淀与缺氧环境密切相关,矿床成因属于沉积变质型.东昆仑地区蓟县系狼牙山组分布广泛,该矿床的发现不仅可带动青海省铁锰矿的勘查和研究,而且进一步拓展了中元古代锰矿的勘查地域范围.Abstract: The sedimentary-metamorphic manganese deposit is an important type of mineral deposit in China and abroad. The Hongshuihe iorn-manganese deposit is the important discovery for Iorn-Manganese ore prospecting in Eastern Kunlun recently. Based on the study about the geological background and the deposit characteristics of Hongshuihe iorn-manganese deposit, the main achievements are obtained as follows. This deposit is located in Jixianian Langyashan Formation, and the ore-body is controlled by stratigraphic position and lithology. It is formed in anoxic environment through the debris deposition, hydrothermal sedimentary, metamorphic and supergene oxidation, which belongs to sedimentary-metamorphic deposit. The discovery of Hongshuihe deposit not only can actuate the exploration and research works of iron-manganese ore in Qinghai Province, but also can expand the prospecting area of Mesoproterozoic manganese deposit.