Krosno(西里西亚)带、乌克兰喀尔巴阡山脉Dukla带古近系Flysch序列和西喀尔巴提亚山脉Intra-Carpathian序列的石英晶体“Marmarosh钻石”形态比较

Q3 Earth and Planetary Sciences
V. Olexandr, Naumko Ihor, Zankovych Halyna, Kuzmenko Yaroslav
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引用次数: 0

摘要

对乌克兰喀尔巴阡山脉Krosno(Silesian)单元复理石矿床矿脉中的“Marmarosh钻石”型石英晶体(137颗晶体,位置1–New Beskydy Tunnel)和Dukla带渐新世沉积物(77颗晶体;位置2–Pryslip pass)进行了角度测量研究。它们与斯洛伐克喀尔巴阡山脉西部喀尔巴提亚山脉内古近纪序列的石英晶体(175颗晶体;位置3–Šoltysa溪流)进行了比较。对所得结果的分析表明,所研究的乌克兰和斯洛伐克地区的“Marmarosh钻石”大体相似。主要的简单形式表示六角棱镜m{101 \ 0}和菱形r{101 \}和z{011 \ 1}。已经确定了以下类型的结晶习性:六方双锥、假三棱柱、六方棱柱、三棱柱。对于乌克兰喀尔巴阡山脉的多面体来说,次要的形式不太典型,例如三角双锥体s{112}和梯形x{516}。据统计,来自乌克兰喀尔巴阡山脉的“Marmarosh钻石”晶体的形状更接近等距。对他们来说,沿着主结晶轴的延伸甚至不如斯洛伐克地区的多面体典型。此外,斯洛伐克W.喀尔巴阡山脉的“Marmarosh钻石”更经常被压扁在{101õ0}处。在晶体生长过程中,随着温度的降低,生长习性由六方双锥向三方棱柱转变。乌克兰喀尔巴阡山脉Krosno(西里西亚)带的石英与方解石共生。这两种矿物中都含有大量的碳氢化合物包裹体。矿物学结晶学和地球化学研究(尤其是迁移的碳氢化合物流体)对喀尔巴阡山含油气省的油气地质具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Comparison of morphology of quartz crystals – “Marmarosh diamonds” – from Paleogene Flysch sequences of Krosno (Silesian) Zone, Dukla Zone in Ukrainian Carpathians, and Intra-Carpathian sequences of Western Carpathians
Quartz crystals of “Marmarosh diamonds” type were goniometrically studied in Ukrainian Carpathians from the veins in flysch deposits of Krosno (Silesian) unit (137 crystals, locality 1 – New Beskydy Tunnel) and the Oligocene sediments of the Dukla Zone (77 crystals; loc. 2 – Pryslip pass). They were compared with quartz crystals from intra-Carpathian Paleogene sequences of the Western Carpathians in Slovakia (175 crystals; loc. 3 – Šoltysa stream). The analysis of the obtained results allows to state that the “Marmarosh diamonds” from the studied Ukrainian and Slovak localities are generally similar. The main simple forms represent the hexagonal prism m {101̅0} and the rhombohedra r {101̅1} and z {011̅1}. The following types of crystal habit have been identified: hexagonal-dipyramidal, pseudocubic, hexagonal-prismatic, trigonal-prismatic. For the polyhedra from the Ukrainian Carpathians, minor forms are less typical, such as the trigonal dipyramid s {112̅1} and the trapezoid x {516̅1}. Statistically, the shape of “Marmarosh diamond” crystals from the Ukrainian Carpathians is closer to isometric. For them, elongation along the main crystallographic axis is even less typical than for polyhedra from the Slovak localities. In addition, “Marmarosh diamonds” from the W. Carpathians in Slovakia are more often flattened at {101̅0}. In the process of crystal growth with decreasing temperature, the habit changes from hexagonal-dipyramidal to trigonal-prismatic. Quartz from Krosno (Silesian) zone of Ukrainian Carpathians was found in the association with calcite. There are numerous hydrocarbon inclusions in both minerals. The mineralogical crystallographic and geochemical investigations (especially of the migrating hydrocarbon fluids), are important for oil and gas geology of the Carpathian oil and gas-bearing province.
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来源期刊
Mineralia Slovaca
Mineralia Slovaca Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology
CiteScore
0.60
自引率
0.00%
发文量
0
期刊介绍: Mineralia Slovaca is a scientific peer-reviewed journal, published by the State Geological Institute of Dionýz Štúr in printed and online versions. The journal publishes original scientific papers, expanding the boundaries of knowledge within the geosciences. It is issued since 1969. Archive of articles on Mineralia Slovaca website enables the online access to full-text papers of all previous years.
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