关于乌克兰喀尔巴阡山脉skyba地区的party - coloured ru矿化的问题

L. Heneralova, O. Kostyuk, L. Khomyak
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引用次数: 0

摘要

乌克兰喀尔巴阡山脉Skyba带古近系岩石的远洋和双远洋(深海)组合特点是远端浊积岩和(双)远洋岩相互穿插。奇特层属于露头中一定层次的岩石。层位的巨大发育,海岸线的长度,这些系统的联运连通性与铜、锰和硫矿化的某些含元素((Fe, Mn), Ni, Cu, Co)的地形物组。无论如何,这一专题需要进一步研究,因此,本章提出的决议草案为时过早。根据需要,将古近系岩石的岩性、结构和结构特性按其他维度进行分解,将有助于阐明它们的意义、理论方面,并了解乌克兰喀尔巴阡山脉的Skyba地带(喀尔巴阡山脉飞陆盆地的外围,靠近Tetis洋)的创造功能。然而,仍有必要进一步开发矿产勘探机会,因为这些矿化也具有经济利益。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The question about partycoloured rud mineralisation in skyba zone of the Ukrainian Carpathians
The pelagical and gemipelagical (deep sea) association peculiarities of Paleogene rocks in the Skyba zone of the Ukrainian Carpathians has distal turbidites and (gemi)pelagites which are interspersed among themselves. Peculiarities horizons belong to a certain levels rocks in outcrops. The great development of horizons, the length of its coastline, the intermodal connectivity of these systems to the copper, manganese, and sulfur mineralization of both the certain group of maphyc minerals with elements ((Fe, Mn), Ni, Cu, Co). In any event, the topic required further study, and the draft resolution proposed in the art was therefore premature. Lithological, structural and textural peculiarities of Paleogene rocks with a breakdown by other dimensions, as required, would help to clarify their meaning, theoretical aspects, and understand function of creation in the Skyba zone of the Ukrainian Carpathians (outer part of the Carpathian flysh basins by Tetis ocean). Nevertheless, there is still a need to develop further opportunities for mineral exploration because these mineralization too are of economic interest.
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