首页> 外文期刊>Clay science >AN INTERSTRATIFIED ILLITE/SMECTITE MINERAL VEIN FOUND IN CHAOTIC ROCK FROM THE NIKORO GROUP IN THE ACCRETIONARY TOKORO BELT, NORTHEASTERN HOKKAIDO, JAPAN
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AN INTERSTRATIFIED ILLITE/SMECTITE MINERAL VEIN FOUND IN CHAOTIC ROCK FROM THE NIKORO GROUP IN THE ACCRETIONARY TOKORO BELT, NORTHEASTERN HOKKAIDO, JAPAN

机译:日本北海道东北部特古罗带尼古罗群的混沌岩中发现的层状伊利石/蒙脱石矿物脉

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摘要

Interstratified illite/smectite mineral was found as a clay vein in the Toyomi landslide-prone area in Kitami City, northeastern Hokkaido, Japan. The white with a slight green tint drusy interstratified illite/smectite mineral vein was observed in chaotic rock of the Nikoro Group in the accretionary Tokoro Belt. The interstratified illite/smectite mineral is associated with calcite, quartz, and chlorite. The mode of occurrence and mineral assemblage indicate that the interstratified illite/smectite mineral precipitated directly from the hydrothermal solution having a near neutral pH.
机译:在日本北海道东北部的北见市,丰臣滑坡易发地区发现了层状伊利石/蒙脱石矿物为粘土脉。在增生的Tokoro带尼古罗集团的混乱岩石中观察到白色,并带有淡绿色的层状伊利石/绿土矿脉。层状伊利石/蒙脱石矿物与方解石,石英和绿泥石有关。发生方式和矿物组合表明,层状伊利石/蒙脱石矿物直接从具有接近中性pH的水热溶液中沉淀出来。

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