中更新世与晚更新世早期的海进较弱，仅有海陆过渡相沉积。
The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from Marine to continental facies...
中更新世与晚更新世早期的海进较弱，仅有海陆过渡相沉积。
The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from marine to continental facies only. The strongest tran…
中更新世与晚更新世早期的海进较弱，仅有海陆过渡相沉积。
The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from Marine to continental facies only...
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.
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.
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