山东省莱西县南墅石墨矿位于胶东隆起栖霞复背斜的南翼，石墨赋存于太古界胶东群旌旗山组刘家庄大理岩段。

Nanshu graphite deposits, located at the south side of Qixia synclinorium in Jiaodong uplift, exist in Liujiazhuang marble member of Jingqishan formation, Jiaodong group of Archaeozic Erathern.

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除了变质程度以外，原岩的类型和碳的原始物质的种类也会影响碳的石墨化作用。

Besides metamorphic grade, the nature of original rocks and the precursor of carbonaceous material may also influence graphitization.

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蔡凹锑矿位于陕豫锑矿带的西段，为矿带中典型的锑矿床。 其控矿岩系主要为秦岭群中部雁岭沟组石墨大理岩。

The Caiwa middle - sized antimony deposit is located on the western Shanxi-Henan antimony ore belt, The hosting rocks are Yanlinggou Formation graphite marble of the Qinling Group.

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