Amoyitele Project

King Solomon’s Amoyitele project is located approximately 150 km northwest of Sonid Zuoqi and within 10 km of the Mongolian border.  It consists of a number of magnetite-rich lode occurrences, some of which are carrying copper carbonate in outcrop.  They are hosted either in Devonian calcareous sediments (skarn style) or in Upper Devonian granite (fault filling).  Later granite porphyry, quartz porphyry and diorite porphyry dykes intrude both the granites and the sediments. 

A former iron-ore mine 230m in strike extent and pitted to a depth of approximately 14m exists immediately south of the southern boundary of King Solomon’s tenement.  The workings strike northwest-southeast directly into King Solomon’s ground.  A scatter of quartz-magnetite vein outcrops and prospecting pits referred to as the Iron Princess prospect occurs approximately 1.5 km north of the southern boundary of the tenement.