Evidence for transforming mineralization of Baiguoyuan silver-vanadium deposit hosted in black shale in Hubei,China

作     者：Hanping Zhuang Jialan Lu Jiamo Fu Jinzhong Liu Chigang Ren Degang Zou 

作者机构：Chinese Acad Sci Guangzhou Inst Geochem Canton 510640 Peoples R China Fudan Univ Dept Phys 2 Shanghai 200433 Peoples R China 

出 版 物：《Chinese Science Bulletin》 (科学通报(英文版))

年 卷 期：1999年第44卷第3期

页      面：263-267页

核心收录：

学科分类：081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 

基　　金：National Natural Science Foundation of China NSFC: 49673190 

主　　题：Baiguoyuan silver-vanadium deposit barite transformation. 

摘      要：Baiguoyuan silver-vanadium deposit is generally thought to be of sedimentary-diagenetic origin. Based on the characteristics of barites, it is suggested that hydrothermal transformation has been involved in mineralization. The barites in black shale can be grouped into irregular ones which were formed during early diagenesis and tabular ones which were formed during late diagenesis. The tabular barites are replaced by pyrite and have formed a regular girdle around them. PIXE analysis states that Ag is greatly concentrated in pyrite replacement girdle. The girdle is the product of hydrothermal transformation. The transformation is one of the main mineralization stages of Baiguoyuan deposit.