摘要
It is considered that Xiapai basic-ultrabasic rock bodies lie in the margin of the older uplift, belonging to western segment of Sankeyushu-Chibaisong arc copper-nickel metallogenic belt. The fold and faulted structure develop especially, and showing olive-norite-gabbro facies in the rock bodies. Ore potential has been preferably found in the basic-ultrabasic rock bodies. Through contrasting with Chibaisong copper-nickel deposit, finding industry ore body is very possible in the study area.