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吉林省磐石市烟筒山镇碱场膨润土矿床地质特征

Geological features of Jianchang bentonite deposit in Yantongshan Town of Panshi City, Jilin Province
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摘要 烟筒山镇碱场膨润土矿床赋存于白垩系下统营城子组流纹岩顶部及安山岩底部的层间接触带部位,为后期热液蚀变层控型矿床。矿石可用于机械铸造和干燥剂等。矿石质量较好,易选,易加工并且开发经济效益好。因此,总结该矿床地质特征,对区域找矿具有指导意义。 Jianchang bentonite deposit of Yantongshan Town occurred in the lower Cretaceous Yingchengzi Formation, the contact zone between rhyolite top and andesite bottom layer, and it is a stratabound deposit of the late hydrothermal alteration. Ores can be used for mechanical casting and drying, etc. Ore quality is good, easy to ore dressing and processing, meanwhile ore has good economic benefits of development. Therefore, the geological features of the ore deposit are summarized, and it has the guiding signiifcance for the regional prospecting.
出处 《吉林地质》 2015年第3期67-69,81,共4页 Jilin Geology
关键词 膨润土矿床 层间接触带 热液蚀变 矿石质量 烟筒山 bentonite deposit contact zone hydrothermal alteration ore quality Yantongshan
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  • 2吉林省磐石市烟筒山镇碱场膨润土矿补充详查报告[R].2008.
  • 3易发成,戴淑霞,侯兰杰,陈廷芳.钙基膨润土钠化改型工艺及其产品应用现状[J].中国矿业,1997,6(4):65-68. 被引量:35

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