摘要
本文以石墨碳同位素的对比研究为主线，结合区域成矿地质特征，提出了豫西南石墨系无机成因的新认识。
The paper put forward a new point of view of graphite being formed by inorganism accordingto comparative research of graphite carbon isopote and regional minerogenetic geological characteristics.
关键词
石墨矿床
碳同位素
无机成因
Graphite deposit Carbon isotope Inorganism genesis
