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Abstract

Investigation site takes place in middle Taurus region, near Kayseri, where ophiolites occupies the whole field. There are numbers of mines, in the area, producing cromite from Anatolian polyform type mineralization nested in ultrabasic rocks situated at the bottom of ophiolitic series.

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/content/papers/10.3997/2214-4609.201408185
1998-06-08
2021-10-16
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408185
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