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Enrichment characteristics of Cu and Co displayed by low-density geochemical mapping in Zambia

2020; Elsevier BV; Volume: 219; Linguagem: Inglês

10.1016/j.gexplo.2020.106634

1879-1689

Junping Ren, Jie Wang, Libo Zuo, Alei Gu, Hongwei Sun, Kang Xu, HE Fuqing, Chipilauka Mukofu, Alphet Phaskani Dokowe, Ezekiah Chikambwe, Cao Shu-ping, Xujiang Cheng,

Heavy metals in environment

The Sino–Zambian Cooperation project provides national catchment sediment geochemical data for 58 elements including Cu and Co from 746 sediment samples at 736 sampling sites, corresponding to a sampling density of about 1 site per 1000 km2. The Cu and Co were determined by Inductively Coupled Plasma Mass Spectrometry (ICP-MS) under strict quality control using field duplicates, standard reference materials and analytical replicate samples. The 95% ranges (2.5%–97.5%) of Cu and Co concentrations were from 1.8 to 57.81 × 10−6 and from 0.54 to 22.83 × 10−6, respectively, reflecting locally unevenness distributions. The median values of Cu and Co are 5.77 × 10−6 and 2.98 × 10−6, respectively. The most noticeable anomalous patterns of Cu and Co are distributed between Lusaka and Solwezi (Lufilian Arc Belt) with the trend of increasing concentrations from southeast to northwest. The all spatial distribution patterns of Cu and Co in tectonic units, drainage basins and geomorphological landscapes show good relations with parent rocks, climate, Cu (Co) deposits and smelting plants in Lufilian Arc Belt. The Cu and Co concentrations show metallogenic belts in Mkushi area, between Lusaka and Solwezi areas, and in Livingstone area.