福建黄地铅锌矿地质特征及成因探讨

The Geological Features and Their Causes of Huangdi Lead and Zinc Mine

摘要: 阐述了黄地推覆构造控矿特征，对矿床成因进行探讨。初步认为，伴随黄地推覆构造的形成演化，动力变质热液沿着推覆构造断层破碎带充填、交代，矿质在破碎带初步富集形成矿化带；燕山期岩浆岩沿断裂上侵，含矿岩浆热液对矿化带叠加改造，最终形成动力变质—岩浆热液叠加改造型铅锌矿床。

Abstract: This paper introduces the geological features and their causes of Huangdi Tuifu formation.With the evolution of Huangdi Tuifu formation, the rock fluid ascended and stuffed in the rock-broken area to form the mining belt.The Yanshan magma intruded into the rock rupture to add and alter the mining belt.The lead and zinc mine deposit was formed in this way.