本矿床是赋存于时代较老、变质较深的岩系中的一个品位较富、规模可观的菱铁矿矿床.已有的少数报道多是根据最初的评价报告,以后的详查、填图和评价资料均未能囊括在内.由于路途遥遥能亲赴现场直接观察与研究的人寥寥无几,兹不避累赘,以亲身参加工作之体会与详查资料整理成此文. This deposit is a relatively high-quality and large-scale siderite deposit hosted in the older and denser rock series.The few existing reports are mostly based on the initial evaluation report, Figure and evaluation information are not included.As far away from the scene to go direct observation and research on the scene few people, not to avoid the burden to personally participate in the work experience and detailed information into the article.