位于青藏高原腹地的羌塘盆地是经历了多期构造改造的改造型盆地。
The Qiangtang Basin in the hinterland of the Qinghai-Xizang Plateau is interpreted as a reworked basin which has undergone multiple phases of tectonic reworking.
持续生烃和压实封闭是普遍超压的主因，现代地压状况是晚期构造改造的结果。
The superpressures mainly result from sustained hydrocarbon-generation and compaction seal and the current geopressure circumstances are the result caused by late tectonic movements.
在经历后期构造改造后，盆地的晚期生烃及晚期油气运移受改造后的构造格局控制。
After the late structural transformation, the late sourcing period and the late oil and gas migration in the basin are controlled by post-transformation structural configuration.
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