Metabasites along the Lunvozh river (Middle Timan): petrography, mineralogy, petrochemistry

A. Shmakova
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Abstract

A small dike of unknown age was found on the territory of the Kanin-Timan region within the Middle Timan along the Lunvozh river. Our studies revealed that the rocks, composing this intrusive body, corresponded to basaltic andesites according to the content of the main rock-forming elements. They were almost completely recrystallized and composed of chlorite (30—40 %), carbonates (25—40 %), albite (10—15 %), quartz (10—15 %), muscovite (5—8 %) and plagioclase (less than 1 %). Accessory minerals were represented by apatite, monazite and rutile. Ore minerals included pyrite, chalcopyrite, and cobaltine. According to the mineral composition and petrochemical characteristics, the rocks composing the dike body along the Lunvozh river, differed from the basites of the Middle Riphean Middle Timan and Devonian Kanin-Timan complexes identified in the Kanin-Timan region.
伦沃日河(中提曼河)沿岸的玄武岩:岩石学、矿物学、岩石化学
在中提曼地区的卡宁-提曼地区,沿着伦沃日河,发现了一个年代不详的小堤坝。根据主要造岩元素的含量分析表明,构成该侵入体的岩石属于玄武岩安山岩。它们几乎完全重结晶,由绿泥石(30 - 40%)、碳酸盐(25 - 40%)、钠长石(10 - 15%)、石英(10 - 15%)、白云母(5 - 8%)和斜长石(不到1%)组成。副矿物以磷灰石、独居石和金红石为代表。矿石矿物包括黄铁矿、黄铜矿和钴矿。根据矿物组成和石油化学特征,构成Lunvozh河沿岸脉体的岩石与卡宁-提曼地区识别的中日番-中提曼和泥盆系卡宁-提曼杂岩的基底不同。
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