黄金科学技术 ›› 2018, Vol. 26 ›› Issue (3): 261-269.doi: 10.11872/j.issn.1005-2518.2018.03.261
• 矿产勘查与资源评价 • 下一篇
杜胜江1,2,温汉捷3,4*,秦朝建3,卢树藩1,燕永锋5,杨光树5
DU Shengjiang 1,2,WEN Hanjie 3,4,QIN Chaojian 3,LU Shufan 1,YAN Yongfeng 5,YANG Guangshu 5
摘要: 对三保锰银矿床进行了系统的碳氧同位素及电子探针研究,发现矿石中的菱锰矿和共生方解石的碳同位素值均偏负,氧同位素值为正,而围岩的碳同位素组成在零值附近。研究结果表明:三保锰银矿床的碳可能主要来自地幔源或深部岩浆系统,但是其碳同位素组成并没有完全落在深部地幔δ13C的范围,暗示着成矿流体中的碳除了主要来源于深部系统之外,还加入了部分大气降水循环淋滤围岩中的碳。该矿床的矿体展布形态以似层状、透镜状和囊状为主,而并非规则层状。另外,微区矿物学还发现矿石中还有少量的典型岩浆型副矿物,如锆石和金红石等。上述研究结果表明,该矿床应属于热液成因,而非一般的海相沉积型。该研究成果不仅阐述了锰银矿床的稳定碳氧同位素特征,而且有助于深化对矿床成因的认识,丰富找矿信息,从而提高找矿效果。
中图分类号:
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