On the basis of O,Pb and C isotopic studies of many gold deposits in western Henan,The authors suggest that the ore-forming fluid of gold deposits is deep flow.

• 通过对豫西众多金矿床的氧、铅、碳同位素的研究，认为豫西金矿的成矿流体是一种在长期地质演化过程中形成的广泛均一化的深部地壳流体。