1) Huangniling granite
黄泥岭岩体
1.
It has been thought that the “Caledonian” granitic intrusions were wi dely distributed in the intersection of northern marginal of the North China Cra ton and the Xing’an-Mongolian orogenic belt, with the Huangniling granite as t he most typical one.
在华北地台北缘与其北侧兴蒙造山带的结合部位 ,发育有大量的所谓“加里东期”花岗岩 ,其中以出露在吉林省中部的黄泥岭岩体最为典型。
2) the Huangling formation
黄岭岩组
1.
Gneissic granitic rocks of the Huangling formation in western Guangdong are the basement metamorphic series (2600Ma -1700 Ma ).
粤西黄岭岩组片麻状花岗质岩石属于云开地块的基底岩系（2600Ma～1700Ma），自下而上发育3种构造样式：下部透入性剪切变形带；中部平直均匀变形带；上部为揉皱带。
4) Siling pluton
泗岭岩体
5) Fuling mass
伏岭岩体
1.
Petrology and geochemistry of the Fuling mass in Jixi, southern Anhui;
皖南绩溪伏岭岩体岩石地球化学特征
6) Huangling (Kongling) complex
黄陵(崆岭)杂岩
补充资料：青泥岭
1.岭名。在今甘肃省徽县南。历来为甘陕入蜀之要途。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条