MVT铅锌矿特征及其对富乐地区铅锌矿形成的启示  

Characteristics of MVT Lead-Zinc Deposits and Their Implications for the Formation of the Upper Permian Yangxin Formation Lead-Zinc Deposits in the Fule Area

作　　者：黄灿奇 董少峰 Huang Canqi;Dong Shaofeng(School of Earth Sciences and Technology,Southwest Petroleum University,Chengdu 610500)

机构地区：[1]西南石油大学地球科学与技术学院,四川成都610500

出　　处：《石化技术》2025年第1期97-99,共3页Petrochemical Industry Technology

摘　　要：密西西比河谷型(MVT)铅锌矿床是世界上重要的铅锌矿床类型之一,为世界铅锌资源储量作出巨大贡献。MVT铅锌矿床一直得到许多学者的关注。主要从MVT铅锌矿床的围岩蚀变特征、成矿年代构造特征、地球化学特征、流体驱动模型等方面进行介绍,并结合富乐铅锌矿区的相关特征进行讨论。研究表明,矿床形成与围岩的蚀变特征、成矿年代和构造环境密切相关。The Mississippi Valley-type(MVT)lead-zinc deposit is one of the world's important types of lead-zinc deposits,contributing significantly to global lead-zinc resource reserves.Over the past few decades,MVT lead-zinc deposits have garnered considerable attention from scholars.This paper reviews previous research and introduces aspects such as the alteration characteristics of the surrounding rock,mineralization age and structural features,geochemical characteristics,andfluid driving models.It also discusses the related characteristics of the Fule lead-zinc mining area.The research indicates that the formation of the deposit is closely related to the alteration characteristics of the surrounding rock,mineralization age,and structural environment.

关 键 词：MVT 围岩蚀变 地球化学 流体驱动模型 

分 类 号：P618.4[天文地球—矿床学]