乌克兰喀尔巴阡山脉Krosno地区(新Beskydy铁路隧道区)矿床中细脉浸渍矿化的非矿石矿物

I. Naumko, H. Zankovych, Oksana Koкhan, Olexander Vovk, Ya. Kuzemko, Bohdan Saкhno, R. Serkiz
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摘要

新的Beskydy铁路隧道的建设揭示了乌克兰喀尔巴阡山脉的Krosno组的本地矿床,为在Krosno构造相单元内的另一个有前景的复理石组含油气区域的研究提供了新的结果。在乌克兰有第二条长度相同的隧道,穿过乌克兰喀尔巴阡山脉的Verkhovyna分水岭山脊。其剖面以Krosno组的岩石为代表,即砂岩、泥质岩和粉砂岩的分层。在这里发现了两个裂隙带,其中矿质(硫化物)和非矿质(方解石和石英型“马尔马罗什钻石”)矿物的脉状浸渍矿化发育。方解石和石英形成单矿物矿脉和共生方解石-石英型的“马尔马罗什钻石”-硫化物。石英以拼接砂的形式出现,多面晶体,透明,黄色,棕色,黑色,绿色。乳白色,半透明的方解石,呈脉状,细脉状,浸渍在石英上的粉末。含有大量的镁、锰和铁杂质,这意味着存在菱镁矿-菱铁矿成分。烃类流体存在于“马尔马罗什钻石”类型的所有方解石和石英晶体中。从化学成分上看,它是含有高级碳氢化合物(最高达己烷)杂质的甲烷。研究了乌克兰喀尔巴阡山脉Krosno地区(Beskydy铁路隧道新支路施工区域)复立石组岩石杂岩,有时记录了细脉浸染矿化裂缝中流出带有油味的黑色物质的表现,具有重要的成因意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Non-ore minerals of veinlet-impregnated mineralization in the deposits of the Krosno zone of the Ukrainian Carpathians (district of the new Beskydy railway tunnel)
The construction of the new Beskydy railway tunnel, which revealed the indigenous deposits of the Krosno formation of the Ukrainian Carpathians, provided an opportunity to obtain new results from the study of another prospective oil and gas-bearing areas of the flysch formation within the Krosno structural-facies unit. There is a second tunnel in length in Ukraine and passes under the Verkhovyna watershed ridge of the Ukrainian Carpathians. Its section is represented by the rocks of the Krosno formation, namely the stratification of sandstones, argillites and silt stones. There are two fracture zones have been indentified here, in which developed veinle-impregnated mineralization of ore (sulfides) and non-ore (calcite and quartz type of the “Marmarosh diamonds”) minerals. Calcite and quartz formas monominerals veins and in paragenesis calcite-quartz type of the “Marmarosh diamonds” ‒ sulfides. Quartz occurs in the form of splice sand well-faceted crystals, transparent, in yellow, brown, black, green colour. Calcite of a milky, translucent colour in the form of veins, veinlets, impregnation, powder on quartz, druz. Contains significant impurities of magnesium, manganese and iron which means the presence of a rhodochrosite-magnesite-siderite component. Hydrocarbon fluids are present in all calcite and quartz crystals of the “Marmarosh diamonds” type. By chemical composition, it is methane with impurities of higher hydrocarbons (up to hexane). Sometimes the manifestations of the outflow of a black substance with the smell of oil from the cracks in the veinlet-impregnated mineralization are recorded studied rock complexes of the flysch formation of the Krosno zone of the Ukrainian Carpathians (construction area of the new branch of the Beskydy railway tunnel), which acquires an important genetic significance.
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