摘要
泗洋铅锌矿产于南园组第三段中酸-酸性火山碎屑岩中,矿体呈透镜状、脉状,受断裂构造、火山环状构造控制。成矿与中生代岩浆侵入及火山活动紧密相关,为中低温岩浆-火山热液型矿床。
The Siyang lead-zinc deposit is discovered in the intermediate acid and acidic volcanoclastic rock of the Late Jurassic Nanyuan Formation. The orebody, with a lenticular or veiny form, is controlled by the faulted structures and volcano ring structures. The metallogenesis of the deposit has a close relation with Mesozoic magmatic intrusion and volcanic activity. It belongs to the deposit of intermediate and low temperature magmatic and volcanic hydrothermal type.
出处
《福建地质》
2008年第3期259-266,共8页
Geology of Fujian
关键词
铅锌矿
地质特征
成因探讨
莆田泗洋
lead-zinc ores, geologic characteristics, genesis, Putian City
