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石平川钼矿由燕山晚期第四次侵入碱性长石花岗岩体提供物源和热动力,火山机构、断裂和西山头组第二岩性段为成矿提供了导矿通道和容矿场所。
The Shihchuanchuan molybdenum deposit is sourced and thermodynamically powered by the fourth intrusive alkaline feldspar granite in the late Yanshanian period. Volcanic structures, faults and the second lithologic section of the Xishantou Formation provide ore-entry channels and ore-hosting sites for mineralization.