Spread Of Laterite Nickel Based on Drill Data at PT Manunggal Sarana Surya Pratama, Southeast Sulawesi Province

Muhammad Aswadi, Jamal Rauf Husain, A. Gazali, Alam Budiman Thamsi
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引用次数: 5

Abstract

Modeling of nickel laterite resources is intended to determine the distribution of resources represented in the form of block models. The results of resource modeling indicate the shape and distribution of mineral deposits which can facilitate the mining process and can predict mining boundaries referring to the results of resource modeling. The purpose of this study was to determine the thickness of the saprolite zone layer and the distribution direction of nickel laterite based on drill point data. The data used in the laterite nickel resource modeling are exploration drill data, drill coordinates, and exploration grade classification. Data processing and analysis methods apply block modeling and the variogram method to determine the distribution direction of nickel resources. Based on the results of the cross-section profiles in Section 1 to Section 7, the average thickness of saprolite is 6,605 m, and the block model layer of saprolite which shows high levels of red color (Ni 1.9 - so on) is the most in the north, pink color (Ni 1.5-1.89) is in the north direction before the Ni 1.9 level above, the green color (Ni 1.3-1.49) is in the east and south.
基于苏拉威西省东南部Manunggal Sarana Surya Pratama PT钻探资料的红土镍扩散
红土镍矿资源建模旨在确定以块模型形式表示的资源分布。资源建模结果显示了矿床的形状和分布,为采矿过程提供了方便,并可根据资源建模结果预测采矿边界。本研究的目的是根据钻孔点资料确定腐岩带层厚度和红土镍矿的分布方向。红土镍资源建模使用的数据是勘探钻井数据、钻井坐标和勘探品位分类。数据处理和分析方法采用区块建模和变差法确定镍资源的分布方向。根据剖面1 ~剖面7的剖面结果,腐岩的平均厚度为6605 m,北部为红色(Ni 1.9—等)水平较高的块状模式层,在Ni 1.9以上水平之前,北部为粉红色(Ni 1.5—1.89),东部和南部为绿色(Ni 1.3—1.49)。
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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