Exploration results have proved that newly found reservoirs are largely dist ributed in the laumontite secondary pore zone. 勘探结果证实延长统找到的油藏大部分都聚集在这些浊沸石次生孔隙中。
The relative high-permeability zones were resulted from the dissolution of authigenic laumontite on the low-permeability background. 该储层由于次生浊沸石溶解在低渗透背景上而形成了相对高渗区。
