深水区储层至少有三套，始新世陆相地层、下渐新统海陆过渡相地层和上新统及其以上海相深水扇。
There are at least three reservoir cases in deepwater: Eocene terrestrial formation, low Oligocene transitional formation and Pliocene and above Marine deepwater fans.
该盆地古近系发育有始新统、渐新统两套地层层序。
The Paleogene series developed Eocene series and Oilgocene series in this basin.
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