摘要
The Xing'an Block (XB) is located between the Erguna
Block (EB) and the Songnen Block (SB), which
topographically occupies the northeastern half of the Great
Xing'an Range (Liu et al., 2017). The XB was
traditionally considered to be composed of a Precambrian
metamorphic basement and post-Cambrian cover.
However, the recent geochronological studies show that
the so-called "Precambrian metamorphic rocks^^ are much
younger in age and considered to be formed in the Early
Paleozoic, indicating no existence of the Precambrian
metamorphic basement.
基金
supported by the China Geological Survey (grant No. DD20160047-02)
the Young Scientists Fund of Shandong Province (grant No. ZR2016DB08)
the Financial Fund of Shandong Province (grant No. 2017CXGC1604)