走向北苏门答腊亚齐中部的矿产潜力图:河流沉积物地球化学的光谱区和局部奇异分形分析的贡献及其与岩浆热液Cu和Au矿化的关系

Pub Date : 2022-03-29 DOI:10.1080/25726838.2022.2053376
Thomas Mulja
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引用次数: 2

摘要

摘要英国领导的北苏门答腊项目于1975年至1980年在亚齐中部收集的河流沉积物的地球化学重新评估,采用光谱-面积和局部奇异分形技术,细化了先前确定的异常Cu区域,并描绘了与斑岩Cu和浅成热液Au–Ag矿床相对应的As异常(Au的替代物),以及在20世纪80年代和90年代。此外,将这些方法应用于一家澳大利亚公司在20世纪90年代中期从亚齐中部部分地区采集的河流沉积物样本,可确定与区域地球化学趋势一致的Au、As和Cu异常。整合单一金属富集区以及矿点和结构的分布,揭示了控制浅成热液Au–Ag和斑岩Cu矿化的向北和向东构造-岩浆走廊。上述结果证明了遗留数据在首次通过矿产评估和为未来矿产远景图提供证据层方面的有用性。
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Toward a mineral potential map of central Aceh, North Sumatra: contributions from spectrum-area and local singularity fractal analysis of stream sediment geochemistry and its relationships to magmatic-hydrothermal Cu and Au mineralisation
ABSTRACT A reassessment of the geochemistry of stream sediments collected by the British-led North Sumatra Project from 1975 to 1980 in central Aceh with spectrum–area and local singularity fractal techniques refines previously determined areas with anomalous Cu and delineates As anomalies (proxy for Au) that correspond to porphyry Cu and epithermal Au–Ag deposits and prospects discovered in the 1980s and 1990s. Additionally, the application of these methods to stream sediment samples collected by an Australian company in the mid-1990s from part of central Aceh identifies Au, As, and Cu anomalies that are aligned with regional geochemical trends. Integrating singularity metal-enriched areas and the distribution of mineral occurrences and structures reveals northerly and easterly tectono-magmatic corridors controlling epithermal Au–Ag and porphyry Cu mineralisation. The above results attest to the usefulness of legacy data for first-pass mineral assessments and for providing evidence layers for a future mineral prospectivity map.
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