Bedding-parallel fractures are fractures that are parallel to rock bedding structure planes and have been widely accepted as a key factor for oil and gas production in tight sandstone and shale reservoirs.However,the ...Bedding-parallel fractures are fractures that are parallel to rock bedding structure planes and have been widely accepted as a key factor for oil and gas production in tight sandstone and shale reservoirs.However,the formation mechanisms of these parallel-bedding fractures are still under debate.In this study,bedding-parallel fractures in Yongjin Oil Field were analyzed using methods including core and microscopic observations,element geochemistry,and carbon and oxygen isotope analysis.Their origin and relations to reservoir quality,faults,and rock mechanical properties were examined.The discovery of bedding-parallel fractures in both the Upper Jurassic and Lower Cretaceous formations indicates that the BPFs are generated later than the early Cretaceous.The filling state of bedding-parallel fractures that with no bitumen and carbonate cement indicate that they formed after oil charging and carbonate cementation.The tensile fracture characteristics in core and thin section observa-tions,and the fact that overburden stress exceeds the pore pressure indicate that the bedding-parallel fractures were neither generated from tectonic compression nor over-pressure.The most likely generation mechanism is stress relief during core drilling under high in situ stress conditions.High in situ stress and low tensile strength lead to thinner fracture spacing.The existence of high bedding-parallel fracture density is an indicator of good reservoir quality and result in high oil/gas production.展开更多
In order to study evolution laws of tensile fractures in a coal mining area, based on the classification of the fractures formed by mining, a physical simulation test was carried out to simulate the dynamic evolut...In order to study evolution laws of tensile fractures in a coal mining area, based on the classification of the fractures formed by mining, a physical simulation test was carried out to simulate the dynamic evolution process of tensile fractures in coal mining areas. The results showed that after the coal in the mining area was mined, the mining area underwent obvious movement and deformation and forms tensile fractures. As the min-ing working face was advanced, the tensile fractures underwent the dynamic process of generation, development and closure. The changing curves of density of tensile fractures with the increase of mining length of the working face liked a ladder （it increased slowly and then rapidly） and then had two peaks （the second peak was higher than the first peak）.展开更多
基金National Natural Science Foundation of China(Grant Nos.41902147,42130813,and 41402117)the Shengli Geophysical Research Institute of Sinopec.
文摘Bedding-parallel fractures are fractures that are parallel to rock bedding structure planes and have been widely accepted as a key factor for oil and gas production in tight sandstone and shale reservoirs.However,the formation mechanisms of these parallel-bedding fractures are still under debate.In this study,bedding-parallel fractures in Yongjin Oil Field were analyzed using methods including core and microscopic observations,element geochemistry,and carbon and oxygen isotope analysis.Their origin and relations to reservoir quality,faults,and rock mechanical properties were examined.The discovery of bedding-parallel fractures in both the Upper Jurassic and Lower Cretaceous formations indicates that the BPFs are generated later than the early Cretaceous.The filling state of bedding-parallel fractures that with no bitumen and carbonate cement indicate that they formed after oil charging and carbonate cementation.The tensile fracture characteristics in core and thin section observa-tions,and the fact that overburden stress exceeds the pore pressure indicate that the bedding-parallel fractures were neither generated from tectonic compression nor over-pressure.The most likely generation mechanism is stress relief during core drilling under high in situ stress conditions.High in situ stress and low tensile strength lead to thinner fracture spacing.The existence of high bedding-parallel fracture density is an indicator of good reservoir quality and result in high oil/gas production.
文摘In order to study evolution laws of tensile fractures in a coal mining area, based on the classification of the fractures formed by mining, a physical simulation test was carried out to simulate the dynamic evolution process of tensile fractures in coal mining areas. The results showed that after the coal in the mining area was mined, the mining area underwent obvious movement and deformation and forms tensile fractures. As the min-ing working face was advanced, the tensile fractures underwent the dynamic process of generation, development and closure. The changing curves of density of tensile fractures with the increase of mining length of the working face liked a ladder （it increased slowly and then rapidly） and then had two peaks （the second peak was higher than the first peak）.
