出露于桐庐冷坞的上石炭统黄龙组、船山组和下二叠统栖霞组、丁家山组,总厚932.3米。
The Huanglong, Chuanshan formation of Upper Carboniferous and the Qixia, Dingjiashan formation of Lower Permian, outcropping in Tonglu-Lengwu, have a total thickness of 932.3 meters.
铜陵花树坡铜矿床主矿体赋存于二叠系下统栖霞组硅质层内,次要矿体赋存于孤峰组内,受层位控制。
The main orebody of Huashupo Copper Deposit in Tongling occurs in silica horizon of Qixia Group of Lower Permian System, while minor ores controlled by strata occur in Gufeng Group.
栖霞组早期海平面开始上升,之后虽然还存在海平面的升降运动,但一直到茅口组末期都一直为开阔台地相。
Although in the early stage of Qixia formation the sea level began to rise, sealevel elevating movement was not stopped until the last stage of Maokou formation, it's still open platform facies.
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.
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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