Nalati mineralization belt is located at Nalati-Hongliuhe suture belt where mineralizing condition is favorable.

Based on the practically-measured field data of Nalati mineralization belt,comprehensive analysis was made of the regional geological characteristics,regional geophysical characteristics,and regional geochemical characteristics of this district and of its relationship with the neighboring districts.

Nalati tectonic belt located between the Ili Basin and the South Tianshan of western Tianshan is 25 km wide, and it is composed of earlier Proterozoic schist, gneiss, migmatite, and migmatitic granite.

Especially,the arc shape structural zone located at the southern margin of the Nalati tectonic belt and Lateral NS trending faults intersecting the .

The article introduces and analyses two new cities, Latina and Sabaudia, inaugurated in Italian Fascist time.

The geochemical characteristics of Nalati median mass and its geological significance;

Nalati tectonic belts as the ultimate demise suture of south Tianshan ocean between Tarim plate - Yili-plate, of which basement is composed of lower Proterozoic gneissic metamorphic supracrustal rocks of Nalati rock group and early Proterozoic gneissic granite.