2、

In late Paleozoic, the western borderline belt of the basin were coastal basin located in passive triphibian margin.

晚古生代盆地西部属被动陆缘构造背景上的滨浅海盆地;

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3、

In above-mentioned geotectonic setting, the western borderline and shape of the basin were different, In early Paleozoic, the western borderline belt of the basin were back-arc basin located in Active triphibian margin.

在此构造背景条件下,盆地西界不同时期范围和形态是不同的。早古生代盆地西缘为主动陆缘性质的弧后盆地;

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4、

Development of the faultage controls the geometry conformation and sediment growth of the triphibian mutually depress basin, and it decides the growth characteristics of basin in different area, thus forming some special oil-gas conformation types.

断层的发育控制陆相断陷盆地的几何形态和沉积发育,决定了盆地的不同区带各有其发育特点,并形成其特有的油气藏类型。

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