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Genesis and properties of chromite deposits in Denizli region (Southwestern Anatolia), Turkey

机译:土耳其德尼兹利地区铬铁矿沉积物的成因及性质

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Chromite deposits are common in the Denizli region, the Southwestern Anatolia. Chemical and mineralogical studies have shown that these deposits are the of the Alpine-type, and the Acoje-type podiform chromites. They have primary relations with the host harzburgite with a thin dunite cover around chromite bodies, which suggests that a wall rock and melt interaction played an important role in the formation of chromite ores.
机译:铬铁矿沉积物在安纳托利亚西南部的Denizli地区是常见的。化学和矿物学研究表明,这些沉积物是高山型和Acoje型植入染色铬酸盐。它们与宿主Harzburgite具有初步的关系,铬铁矿体周围有薄的Dunite盖,这表明壁岩和熔体相互作用在铬铁矿矿石的形成中发挥了重要作用。

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