Jiaobei Belt 胶北带
Jiaobei area 胶北地区
Jiaobei uplift 胶北隆起区
Jiaobei terrane 胶北地体
the Jiaobei massif 胶北地块
Jiaobei uplift belt 胶北隆起带
以上来源于: WordNet
After deposition of the Fenzishan Group, the Fenzishan event finally solidified the basement in the Jiaobei region 1700 .
于粉子山群沉积之后、大致17亿年前发生的粉子山事件使胶北地区基底最后固结。
Lots of mafic - ultramafic enclaves are developed in Neoarchaean TTG gneisses in south of Jiaobei uplift with the trend of NEE.
在胶北隆起南缘新太古代TTG质片麻岩中发育了大量的超铁镁质-铁镁质岩包体,呈NEE向群带状展布。
Jiaodong area is located in the eastern part of Shandong Province, which can be divided into two tectonic units: Jiaobei fault-block and Jiaonan orogenic belt.
胶东地区可划分为两个大地构造单元:胶北断块和胶南造山带。
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