辽宁北部处于内蒙古科尔沁沙地“百里翰海”的南缘。
The northern part of Liaoning Province lies to the south of Kerqin Desert of Inner Mongolia.
它们紧密共生，呈狭长的带状分布于辽宁北部晚前寒武纪造山带内。
The rocks coexist closely, distributing in a narrow and long belt in the Late Precambrian orogenic belt in northern Liaoning.
浑河断裂带位于辽宁省东北部，该区是辽宁的心腹地带。
The fault belt area of Hunhe River is situated in the northeastern part of Liaoning Praince.
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