A series of half graben like faulted basins were developed in Jurassic in the northern edge of Qaidam basin, which was mainly controlled by extensional tectonic framework.

柴达木盆地北缘地区在侏罗纪主要受伸展构造体制控制，发育一系列规模较小的箕状断陷盆地。

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The characteristic geotectonic framework of many depression-faulted bas - ins, made the hydrocarbon distributed as belts.

断陷盆地特有的构造格架，使油气按带分布。

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By the way Binzhou fault, Nehe fault, Sunwu_Shuangliao fault, Centren fault and so on controlled tectonic framework especially distribution of faulted basin.

此外，盆地的滨州断裂、讷河断裂、孙吴双辽断裂、中央断裂等壳断裂，对滨北地区的构造格局，尤其是断陷期断陷盆地的展布起控制作用。

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