准噶尔盆地腹部地区深层砂岩储层孔隙特征研究
THE RESERVOIR CHARACTERISTIC OF DEEPLY-BURIED SANDSTONE IN THE CENTER OF JUNGGAR BASIN
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摘要: 准噶尔盆地腹部地区目前已发现的油气多集中在侏罗系和白垩系砂岩中,储层埋深主要在3500~6200m左右,目前储层处于晚成岩阶段A期,砂岩储层主要发育粒间溶蚀孔隙,次生孔隙度主要分布在4%~20%之间,主要是烃源岩成熟产生的有机酸对碳酸盐胶结物和硅酸盐颗粒溶蚀形成的。根据温度—深度—成熟度之间的对应关系推测,由于有机酸在高温下可转化成CO2,因此垂向上发育的另一个次生孔隙带大约在6500m以下,主要是溶解含铁碳酸盐胶结物所致。Abstract: Many discovered petroleum mainly develop in the deeply-buried Jurassic and Cretaceous sandstone reservoirs in the center of Junggar Basin and intergranular secondary porosity develop at the depth of 3 500~6 200 m belong to a stage of late diagenesis. The porosity is about 4%~20% resulting from organic acid that generates from hydrocarbon maturation dissolving carbonate cements and silicate. According to the relationship among temperature, depth and Ro (vitrinite reflectance), there exists the other small scale secondary porosity band vertically resulting from organic acid dissolving ferro carbonate cements at the depth of 6 500 m.
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