2) Songliao Massif
松辽地块
3) Jiao-Liao-Korea block
胶辽朝块体
1.
In the Sinian(680Ma ),the Sino-Korean plate began to break up into two different tectonic units,the Jiao -Liao -Korea block(JLKB)and North China block(NCB).
华北块体(NCB)与胶辽朝块体(JLKB)是中朝板块东部从震旦纪(680Ma)开始裂解的两个不同的构造单元。
4) the Jiaobei massif
胶北地块
1.
Phase equilibria and p-T path of high-and low-pressure pelitic granulites from the Jiaobei massif;
胶北地块高压与低压泥质麻粒岩的相平衡关系与p-T演化轨迹
5) Jiaoliao Luxi and Xuhuai area
胶辽鲁西徐淮地区
1.
According to study on rock property combination, palaeobio characteristics and sesmic event strata, Neoproterozoic strata in Jiaoliao Luxi and Xuhuai area can be multi-divided and contrasted as follows: Heishanguan formation and Erqingshan formation in Luxi area are conformity with Diaoyutai formation and Nanfen formation, while Baoshankou fomation can contrast with Nanfen formation.
依据岩性组合、古生物特征及地震事件层研究 ,对胶辽鲁西徐淮地区新元古代地层可作如下多重划分对比 :鲁西黑山官组、二青山组分别与辽东的钓鱼台组、南芬组相当 ,胶东豹山口组可与南芬组对比 ,它们同属青白口系。
6) Songliao plate
松辽板块
1.
Therefore, Songliao plate seems to be a large-size alloch.
所以 ,松辽板块是大型移置体 ,而大兴安岭则是松辽板块与蒙古板块 (兴蒙古生代褶皱系 )挤压碰撞活动的产
补充资料：白辽辽
1.见"白??4A4D"。
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