碳酸盐岩潜山油藏储层孔隙主要为裂缝和溶洞，其中溶洞是主要的储集空间，裂缝是主要的渗流通道。
The reservoir pore of carbonate buried-hill reservoir is fracture and cavern mostly. The cavern is the primary reservoir space and fracture is the primary seepage channel.
探索了用地层倾角、长源距声波、电阻率、三孔隙度及蚀变系数识别储集空间类型以及对储层分类的方法；
The methods to identify the types of reservoir by using such parameters as dipmeter, long space sonic, resistivity, porosity and alteration factor are studied.
通过玄武岩储层主要成岩作用与孔隙演化的研究，分析其对玄武岩储集空间的影响。
Through the research the mainly Diagenesis and porosities, dissolved caverns, fissures evolutions of the basalt reservoir, we analytical their influences to reservoir spaces properties.
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