Linking mineralogical, geochemical, and textural controls to petrophysical signatures in the Kiruna Mining District, Sweden

Ervin Veress , Oskar Rydman , Rayhan A. Farrenzo , Joel B.H. Andersson , Mathis Warlo , Irvine R. Annesley , Tobias E. Bauer
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Abstract

Discoveries of deposits at shallow depths are becoming scarce, leading exploration efforts to increasingly focus on deeper targets. Traditional exploration techniques for subsurface mapping are often ineffective in terrains obscured by vegetation and glacial sediments, prompting the development of new methods, particularly those centered on geophysics. While geophysical surveys can be valuable for peering beneath the surface cover, reducing initial exploration costs, they are often insufficient to resolve the three-dimensional architecture in structurally complex settings. Integrating geological and geophysical studies ensures that geological characteristics of rock units and structural frameworks are considered, leading to geologically validated results. Merging geological and geophysical models demands a strong understanding of how physical properties are distributed and influenced by geological factors. Our study aims to enhance the understanding of geological factors controlling petrophysical properties in the Kiruna Mining District (Sweden). We conducted an integrated analysis of geochemistry, mineralogy, texture, and petrophysical properties from 35 outcrop locations, including 105 density, magnetic susceptibility, and P-wave velocity measurements from the Kiruna area. The results reveal not only distinct contrasts between lithological units but also significant intraformational variability driven by alteration and fabric, which can obscure lithological boundaries in geophysical surveys. Structural processes such as crustal shortening and basin inversion were found to impose a strong control on the petrophysical properties, contributing to complex and diagnostic signatures. The geological-petrophysical framework presented in this study serves as a foundation for integrated studies in northern Sweden, enabling geophysical methods to serve as a tool for understanding mineral system components and test conceptual models.

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瑞典基律纳矿区的矿物、地球化学和构造控制与岩石物理特征的联系
在浅层发现的矿床越来越少,导致勘探工作越来越多地集中在更深的目标上。在植被和冰川沉积物遮挡的地形中,传统的地下测绘勘探技术往往是无效的,这促使了新方法的发展,特别是那些以地球物理为中心的方法。虽然地球物理调查对于探测地表覆盖下的情况很有价值,可以降低初始勘探成本,但它们往往不足以解决结构复杂环境中的三维结构。将地质和地球物理研究结合起来,可以确保考虑岩石单元和构造框架的地质特征,从而得到地质上有效的结果。合并地质和地球物理模型需要对物理性质如何分布和受地质因素的影响有深刻的理解。本研究旨在加深对瑞典基鲁纳矿区岩石物性控制因素的认识。我们对基鲁纳地区35个露头位置的地球化学、矿物学、结构和岩石物理性质进行了综合分析,包括105个密度、磁化率和纵波速度测量。结果不仅揭示了岩性单元之间的明显差异,还揭示了由蚀变和构造驱动的显著地层内变异性,这可能会模糊地球物理调查中的岩性边界。发现地壳缩短和盆地反转等构造过程对岩石物性有很强的控制作用,有助于形成复杂的诊断特征。本研究中提出的地质-岩石物理框架为瑞典北部的综合研究奠定了基础,使地球物理方法成为理解矿物系统组成部分和测试概念模型的工具。
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