摘要
Graphite has been identified for the first time from rich magnetite ores in Gongehangling,Northeast China.It is suggested that the deposit is originated from siderite of sedimentary origin through regional metamorphism.In view of the unique charaeteristics of its geologieal setting and mineral assemblage this deposit should be elassified as a new type in
Graphite has boon identified for the first time from rich magnetite ores in Gongehangling,Northeast China.It is suggested tliat the deposit i.s originated from siderite of sedimentary origin through regional metamorphism.In view of the unique characteristics of its geological setting and mineral assemblage this deposit should be classified as a new type in China.
出处
《地球化学》
CAS
1979年第2期170-177,共8页
Geochimica