军川断裂是绥滨坳陷的主要控盆断裂，控制了其形成和演化。
Junchuan fault, a magor fault, controlled the formation and evolution of the depression.
绥滨坳陷是三江盆地的次一级构造单元，位于三江盆地的西部。
Suibin depression, as a secondary tectonic unit, lies in the west of Sanjiang basin.
绥滨地区东荣组和绥滨组的建立在区域性对比上建立了一个较完整的晚侏罗世地层柱状。
The establishment of Suibin group and Suibin group in Suibin area build a more completed picture of the late Jurassic stratigraphic column on regional contrast.
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