Gold lodes in the Jichanggouliang gold deposit mainly strike NW and nearly NS and the mineralizing depth of ore bodies in the NW-trending lodes is about 200m, shallower than that in the NS-trending lodes.

Jinchanggouliang gold deposit is located in the Longtan block of the northeasternNuluerhu uplifted belt, which stands at the east of Zhangjiakou – Chifeng gold ore-belt,the northern edge of Huabei platform.

The regional ductile shear zone is well developed in the Huachanggou gold deposit,and it has gone through multiple activities from right-handed earlier to left-handed later and then right-handed latest.

The Huachanggou gold deposit lies in the south of Mianlue Fold bend, in the triangle area of Mianluening , the south of the Qinling Mountain orogenic zone .

Genesis and Significance of Dark Dikes in the Jinchanggouliang Mine Area,Inner Mongolia:Evidences from Geochemistry of the Major and Trace Elements;

Discussin on genesis and geological-geochemical feature of Jinchanggouliang-Erdaogou gold minerogenetic field;

The compositional types of chromium-bearing layered silicate minerals from the Jinchang gold deposit in Mojiang County, Yunnan Province;

Based on a study of fluid inclusions in the Jinchang gold deposits of Heilongjiang Province and a comparison of characteristics of inclusions in rocks with different mineralization intensities,the authors hold that the minera-lization intensity is closely related to the evolution degree of magma and fluid.

The Jinchang gold deposit is located at the junction of Taipingling uplift and Laoheishan depression.

Zircon SHRIMP U-Pb geochronology of the granitoid intrusions from Jinchanggouliang-Erdaogou gold orefield and its significance.;