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Alteration at Kisladag gold mine, Turkey - a progressive study in geology, geotechnics and geometallurgy

机译:凯斯拉格金矿,土耳其的改变 - 地质,岩土科和地质冶金的逐步研究

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The Kisladag Mine, Turkey, is a large porphyry gold deposit which is mined by open pit methods. In operation for over ten years, Kisladag provides an excellent example of how attention to a geologic feature, namely hydrothermal alteration, became a very effective predictive geological tool for planning and operation. The alteration domains were initially used as a geological tool to assist with establishment of resource model domains and to guide delineation drilling, but they were soon recognised to be correlative to geotechnical characteristics (affecting pit slope angles) and metallurgical performance (heap leach recoveries). Recent developments in spectral processing allow the systematic quantification of complex overlapping alteration phases and have greatly improved the ability to rapidly define internally consistent alteration domains for geotechnical and geometallurgical purposes.Alteration at Kisladag comprises a central core potassic (K-feldspar-biotite) zone, a tourmaline-white mica enveloping zone, an advanced argillic lithocap on the deposit's eastern side and an overprinting pervasive argillic zone. These alteration zones and their distribution were based initially on strictly qualitative, visual mineralogical logging of diamond drill core. With the need for more accurate and consistent identification of the alteration mineral suites, particularly the phyllosilicate phases, logging was augmented by systematic measurement of spectral data using a Terraspec instrument.Recently the Kisladag spectral database (over 85000 readings) was reprocessed by the newly developed methodology (aiSIRIS~(TM)) that allows relative quantification of the spectrally-responsive minerals. Visualising this transformed spectral mineralogy at various mineral concentration thresholds using implicit modelling software (Leapfrog~R) led to the creation of consistent mineralogical and alteration domains that are used for the definition of geotechnical and geometallurgical parameters. An implicit modelling workflow enables these domains to be easily updated as new data is collected while maintaining geological integrity of the model.
机译:土耳其凯斯拉格矿,是一种大斑岩金矿床,由露天坑方法开采。在运作超过十年中,kisladag提供了一个很好的例子,即如何关注地质特征,即水热改变,成为规划和运营的非常有效的预测地质工具。改变域最初用作地质工具,以协助建立资源模型域并指导描绘钻探,但是很快被认识到与岩土特征(影响坑坡角)和冶金性能(堆浸出回收)相关。光谱处理中最近的发展允许复杂重叠改变阶段的系统定量,并且大大提高了快速定义岩土和地质冶金的内部一致的改变域的能力。kisladag的alattation包括中央核心牛(K-Feldspar-Biotite)区,矿床东侧的高级野生岩皮划谱,储存的东侧和夸张的普罗旺斯地区。这些改变区域及其分布最初是基于严格定性的钻石钻芯的视觉矿物测井。需要更准确和一致的改变矿泉套,特别是文学阶段的识别,通过使用TretaSpec仪器系统测量光谱数据的系统测量来增强测井。即将通过新开发的Kisladag谱数据库(超过85000读数)进行了再加工允许响应响应矿物的相对量化的方法(AISIRIS〜(TM))。使用隐式建模软件(LEAPFROG〜R)以各种矿物浓度阈值可视化该转化的光谱矿物质,导致了一致的矿物学和改变域,该域用于岩土和几何参数的定义。隐式建模工作流使得这些域能够在保持模型的地质完整性的同时收集新数据时,可以轻松更新。

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