The Chang-63 reservoir in the Huaqing area has widely developed tight sandstone ＂thick sand layers, but not reservoirs characterized by rich in oil＂, and it is thus necessary to further study its oil and gas enrichm...The Chang-63 reservoir in the Huaqing area has widely developed tight sandstone ＂thick sand layers, but not reservoirs characterized by rich in oil＂, and it is thus necessary to further study its oil and gas enrichment law. This study builds porosity and fracture development and evolution models in different deposition environments, through core observation, casting thin section, SEM, porosity and permeability analysis, burial history analysis, and ＂four-property-relationships＂ analysis.展开更多
At present,researches on the pore evolution of shale reservoir and its evolution mechanism are still at such a groping stage that a consensus has not yet reached.Based on core analysis and thermal simulation experimen...At present,researches on the pore evolution of shale reservoir and its evolution mechanism are still at such a groping stage that a consensus has not yet reached.Based on core analysis and thermal simulation experiments,the pore types,pore structures and pore-size change rules of shale gas reservoirs of Upper Ordovician Wufeng-Lower Silurian Longmaxi Fms in the southeastern(SE)Sichuan Basin and its basin-margin transition zone(hereinafter referred to as the basin-margin transition zone of SE Chongqing)were studied by means of argon ion polishing-scanning electron microscopy(SEM)and atomic force microscopy.Then,the evolution characteristics of organic pores were discussed,and the influence of associated minerals on pore evolution was analyzed.Finally,a pore evolution model for the shale gas reservoirs in this area was established.And the following research results were obtained.First,three types of reservoir spaces are mainly developed in the high-quality shale reservoirs of Wufeng-Longmaxi Fms in this area,including fracture,inorganic pore and organic pore.And the organic pores provide the primary reservoir space of shale gas,which can be divided into four categories,i.e.,amorphous kerogen pores,structured kerogen pores,asphaltene pores and paleontology fossil pores.Second,organic contracted fractures are related to the contraction of organic matters,first appearing on one side of the organic matters and then becomes wider and wider with the increase of temperatures.Third,organic pores are mostly the“spongy”pores distributed densely inside the organic matters.When Ro is in the range of 1.56-3.50%,macropores and mesopores are dominant.And when Ro exceeds 3.50%,macropores decrease while mesopores and micropores increase.Fourth,the types of organic matters and the content of associated minerals(e.g.clay minerals,siliceous particles and pyrite)play an important role in the development of pores.In conclusion,the pore evolution law of Wufeng-Longmaxi shale in the basin-margin transition zone of SE Chongqing is that with the increase of burial depth,inorganic porosity decreases significantly,organic porosity increases first and then decreases,and the total porosity shows a change trend of decreasing first,then increasing and finally decreasing continuously.展开更多
文摘The Chang-63 reservoir in the Huaqing area has widely developed tight sandstone ＂thick sand layers, but not reservoirs characterized by rich in oil＂, and it is thus necessary to further study its oil and gas enrichment law. This study builds porosity and fracture development and evolution models in different deposition environments, through core observation, casting thin section, SEM, porosity and permeability analysis, burial history analysis, and ＂four-property-relationships＂ analysis.
基金supported by the National Major Science and Technology Project“Demonstration project of normal-pressure shale gas exploration and development in the Pengshui area”(No.2016ZX05061)the Sinopec Science and Technology Development Department Project“Study on main controlling factors of shale gas enrichment in the basin-margin transition zone of SE Chongqing”(No.P18057-2).
文摘At present,researches on the pore evolution of shale reservoir and its evolution mechanism are still at such a groping stage that a consensus has not yet reached.Based on core analysis and thermal simulation experiments,the pore types,pore structures and pore-size change rules of shale gas reservoirs of Upper Ordovician Wufeng-Lower Silurian Longmaxi Fms in the southeastern(SE)Sichuan Basin and its basin-margin transition zone(hereinafter referred to as the basin-margin transition zone of SE Chongqing)were studied by means of argon ion polishing-scanning electron microscopy(SEM)and atomic force microscopy.Then,the evolution characteristics of organic pores were discussed,and the influence of associated minerals on pore evolution was analyzed.Finally,a pore evolution model for the shale gas reservoirs in this area was established.And the following research results were obtained.First,three types of reservoir spaces are mainly developed in the high-quality shale reservoirs of Wufeng-Longmaxi Fms in this area,including fracture,inorganic pore and organic pore.And the organic pores provide the primary reservoir space of shale gas,which can be divided into four categories,i.e.,amorphous kerogen pores,structured kerogen pores,asphaltene pores and paleontology fossil pores.Second,organic contracted fractures are related to the contraction of organic matters,first appearing on one side of the organic matters and then becomes wider and wider with the increase of temperatures.Third,organic pores are mostly the“spongy”pores distributed densely inside the organic matters.When Ro is in the range of 1.56-3.50%,macropores and mesopores are dominant.And when Ro exceeds 3.50%,macropores decrease while mesopores and micropores increase.Fourth,the types of organic matters and the content of associated minerals(e.g.clay minerals,siliceous particles and pyrite)play an important role in the development of pores.In conclusion,the pore evolution law of Wufeng-Longmaxi shale in the basin-margin transition zone of SE Chongqing is that with the increase of burial depth,inorganic porosity decreases significantly,organic porosity increases first and then decreases,and the total porosity shows a change trend of decreasing first,then increasing and finally decreasing continuously.
