Tectonic evolution characteristics of the foreland basin on the southern margin of the Dabie-Sulu orogenic belt;

Zircon ages and Hf isotopic composition of gneisses from the Rongcheng ultrahigh-pressure terrain in the Sulu orogenic belt;

Major and trace element geochemistry of granitic gneisses from Sulu orogen,eastern Shandong Peninsula: evidence for a Neoproterozoic active continental margin in the northern margin of the Yangtze craton.;

Low-grade metamorphic rocks of greenschist facies occurred in the ultrahigh pressure (UHP) metamorphic zone in the Sulu orogen.

Three layers are present in the middle and upper crusts in the northern border of Sulu orogenic belt, as revealed by the S-N-strike reflecting seismic profiles that cross the Zhucheng sag.

High-pressure sinistral strike-slip shear belts in the NE-trending Tan-Lu fault zone along the western margin of the Sulu orogenic belt are first reported in this paper.

Lithostratigraphic framework on the southern margin of the Su-Lu orogen;

According to the synthetic study of regional correlation of metamorphic supracrustal rocks in the orogen, and the sequence of the magmas evolvement and their Nd isotope, it is suggested that the basement of Su-Lu orogeny belongs neither North China block, nor Yangtze block, but an unattached geotectonic unit.

According to detailed mapping in the Jinping area on the southern edge of the Su-Lu orogen, it is affirmed that the boundary between the ultrahigh-pressure metamorphic belt and high-pressure metamorphic belt is a ductile shear zone.

Possible tectonic manifestations of the Dabie-Sulu orogenic belt on the Korean Peninsula;