赤路斑岩钼矿床产于燕山晚期花岗岩岩株的顶部似斑状花岗岩中。这是丽水—政和—大埔深大断裂带东侧、浙闽粤中生代火山岩中发现的第一个大型斑岩型钼矿床。赤路斑岩钼矿床位于寿宁—连江南北向构造、宁德三都沃—崇安下岚头北西向构造和次一级的碧岩—罗洋北东东向断裂火山岩带三者的交汇处。沿碧岩—罗洋断裂火山岩带侵入露 The Chillu porphyry molybdenum deposit was produced on the top of a granite-like granite at the late Yanshanian granitoids. This is the first large-scale porphyry-type molybdenum deposit found in the Mesozoic volcanic rocks on the east side of the Lishui-Zhenghe-Dapu deep big fault zone. The Chilu porphyry molybdenum deposit is located at the intersection of the Shouning-Lienjiang north-north direction, the Ningde Sanduwo-Chong’an Xiaolan head northwestward structure and the next level of the Bi-Luoyang NNE fault volcanic belt Department. Invasion of dew along the biotite-Luo Yang fault volcanic belt