论文部分内容阅读
本区这套陆相地层,上与早二迭世哲斯组呈断层接触,其下又被东苏花岗岩体侵入。因此,这套地层时代的确定,及其和哲斯组关系的解决,不仅直接有助于区测填图的顺利进行,而且可以正确认识内蒙地槽区的地质历史发展和东苏花岗岩体的侵入时代。
The continental strata in this area are in contact with faults of the Early Silizi Formation and are intruded by the East Su-granite. Therefore, the determination of this stratigraphic age and the settlement of its relations with the Jesse Group not only directly contribute to the smooth development of the regional survey maps, but also correctly understand the geological and historical development of the Trench Zone in Inner Mongolia and Invaded the era.