The impact of lithological variability of reservoir rocks on the quality parameters of the Cu-Ag deposit, Lubin–Głogów Copper District (LGCD)

W. Kaczmarek, M. Wasilewska-Błaszczyk, M. Dudek
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引用次数: 2

Abstract

The article discusses the lithological and facies development of the copper ore deposit in the Fore-Sudetic Monocline in the so-called depression at the top of the Weissliegend. The lithological variability and quality parameters of the deposit in the exploitation field located between the Central and Northern elevations of Rudna, where the deposit profile is described as “typical”, i.e. the Cu-Ag mineralization occurs in all three basic lithological types of copper ore, is analyzed. The lithological variability of ores in depression zones is the reason why the degree of mineralization and the parameters of the economic deposit are highly variable. The authors focused on the mutual relationships between the neighbouring lithological units and the development of the balance deposit. To illustrate the variability of deposit parameters closely related to the lithological and facies development of the host rocks, three-dimensional lithological and geochemical models and isoline maps of the thickness of individual specific copper ore types were made using geostatistical methods and based on field observations and sampling of the deposit.
Lubin-Głogów铜区储层岩性变异对铜银矿质量参数的影响
本文讨论了前苏东单斜中所谓的韦斯里格顶坳陷的铜矿床的岩性和相发育。本文分析了位于鲁德纳中部和北部海拔之间的开采矿区的矿床的岩性变异性和质量参数,该矿区的矿床剖面被描述为“典型”,即铜银矿化发生在铜矿石的所有三种基本岩性类型中。凹陷带矿石的岩性变异性是成矿程度和经济矿床参数变化很大的原因。重点讨论了邻近岩性单元与平衡矿床发育之间的相互关系。为了说明与寄主岩石的岩性和相发育密切相关的矿床参数的变异性,利用地质统计学方法,在实地观察和矿床取样的基础上,绘制了个别特定铜矿石类型的三维岩性和地球化学模型和厚度等值线图。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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