RE:NewsFrom this paragraph...
Within the mudstones and debris flows of the targeted Clm unit hosting NGE’s East Golden Gorge target, from 1,150 metres to the bottom of the hole at 1,405 metres, SGVC012 encountered a thick interval of intense de-calcification and brecciation hosting dense silicification with black remobilized carbon veinlets and fine-grained ‘sooty’ pyrite veinlets typical of Carlin-type hydrothermal fluid flow. Importantly, the thickness and intensity of these alteration features is consistent with the massive volumes of hydrothermal fluid flow associated with Nevada’s large Carlin-type gold deposits, and within this unit NGE’s preliminary XRF analyses confirm the presence of highly-anomalous Carlin-type pathfinders at the concentrations known to exist in the bedrock surrounding these large deposits, including a 96-metre interval averaging multi-hundred-ppm arsenic. To this I saw in Mining .com https://www.mining.com/why-gold-loves-arsenic/ You may have to copy and paste the link....Bluetick