The reservoirs mostly exist in the medium-and coarse-grained sandstones deposited from high-energetic deltaic plain distributary channels in the SMTF.
储层主要发育在太二段高能量的三角洲平原分流河道中、粗砂岩中。
The reservoirs mostly exist in the medium-and coarse-grained sandstones deposited from high-energetic deltaic plain distributary channels in the SMTF.
储层主要发育在太二段高能量的三角洲平原分流河道中、粗砂岩中。
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