The Upper Triassic reservoir in west Sichuan foreland basin has experienced normal compaction and ancompaction.

川西前陆盆地上三叠统储层具有正常压实和欠压实两种类型。

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The Upper Triassic reservoir in west Sichuan foreland basin has experienced normal compaction and ancompaction.

川西前陆盆地上三叠统储层具有正常压实和欠压实两种类型。

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