对黄沙坪铅锌矿床内带铁门锌矿的研究表明，其形成的温度为300C土；压力大致为107Pa；fs2约为10(12.36)；fo2约为10(35.14)；pH值约为5．5；pco；约为7．93×104～17．86×104Pa。成矿溶液中Fe和Zn的主要存在形式有：FeCl+、FeOH+、FeCl0、Zn（HS）、ZnCl+、ZnCl以及Fe2+等。铁闪锌矿中Fe2+含量与温度和fs2关系最密切，而后者更为重要。Fe2+是在铁闪锌矿结晶过程中进入八面体位置的一这是ZnS与FeS之间构成有限固港体的根本原因。 The study on iron-bearing zinc-zinc deposits in the Huangshaping Pb-Zn deposit shows that the formation temperature is 300 C, the pressure is about 107 Pa, the fs2 is about 10 (12.36), the fo2 is about 10 (35.14) and the pH is about 5 .5; pco; about 7.93 × 104 ~ 17.86 × 104Pa. The main existing forms of Fe and Zn in ore-forming solution are FeCl +, FeOH +, FeCl0, Zn (HS), ZnCl +, ZnCl and Fe2 +. The content of Fe2 + in the marmatite is most closely related to temperature and fs2, while the latter is more important. Fe2 + is an octahedral site in the crystallization of marzudellite, which is the fundamental reason for the formation of a limited solid body between ZnS and FeS.