陡山沱组的储集空间有晶间孔隙和裂隙缝洞空间。
The reservoir Spaces of the Doushantuo Formation consist of inter crystalline pores and fracture voids.
文中还讨论了陡山沱组的沉积环境及化石的保存。
The sedimentary environment and the fossil preservation of the Doushantuo Formation is discussed in this paper.
陡山沱组盖帽碳酸盐岩形成于温暖条件下、微咸化海水沉积环境，属潮间—潮下台地前缘斜坡和浅海盆地之间的过渡带。
The precipitation of Doushantuo cap carbonates was deposited in warm, brackish water, and between the intertidal-subtidal inner ramp and shallow basin.
陡山沱组盖帽碳酸盐岩形成于温暖条件下、微咸化海水沉积环境，属潮间—潮下台地前缘斜坡和浅海盆地之间的过渡带。
The precipitation of Doushantuo cap carbonates was deposited in warm, brackish water, and between the intertidal-subtidal inner ramp and shallow basin.
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