Matches in SemOpenAlex for { <https://semopenalex.org/work/W3211119963> ?p ?o ?g. }
- W3211119963 endingPage "569" @default.
- W3211119963 startingPage "554" @default.
- W3211119963 abstract "Core, thin section, conventional and image logs are used to provide insights into distribution of fractures in fine grained sedimentary rocks of Permian Lucaogou Formation in Jimusar Sag. Bedding parallel fractures are common in fine grained sedimentary rocks which are characterized by layered structures. Core and thin section analysis reveal that fractures in Lucaogou Formation include tectonic inclined fracture, bedding parallel fracture, and abnormal high pressure fracture. Bedding parallel fractures are abundant, but only minor amounts of them remain open, and most of them are partly to fully sealed by carbonate minerals (calcite) and bitumen. Bedding parallel fractures result in a rapid decrease in resistivity, and they are recognized on image logs to extend along bedding planes and have discontinuous surfaces due to partly-fully filled resistive carbonate minerals as well as late stage dissolution. A comprehensive interpretation of distribution of bedding parallel fractures is performed with green line, red line, yellow line and blue line representing bedding planes, induced fractures, resistive fractures, and open (bedding and inclined) fractures, respectively. The strike of bedding parallel fractures is coinciding with bedding planes. Bedding parallel fractures are closely associated with the amounts of bedding planes, and high density of bedding planes favor the formation of bedding parallel fractures. Alternating dark and bright layers have the most abundant bedding parallel fractures on the image logs, and the bedding parallel fractures are always associated with low resistivity zones. The results above may help optimize sweet spots in fine grained sedimentary rocks, and improve future fracturing design and optimize well spacing." @default.
- W3211119963 created "2021-11-08" @default.
- W3211119963 creator A5002273544 @default.
- W3211119963 creator A5011560454 @default.
- W3211119963 creator A5012411460 @default.
- W3211119963 creator A5041989475 @default.
- W3211119963 creator A5069168874 @default.
- W3211119963 creator A5076757967 @default.
- W3211119963 creator A5079732143 @default.
- W3211119963 date "2022-04-01" @default.
- W3211119963 modified "2023-10-14" @default.
- W3211119963 title "Bedding parallel fractures in fine-grained sedimentary rocks: Recognition, formation mechanisms, and prediction using well log" @default.
- W3211119963 cites W1120298015 @default.
- W3211119963 cites W1942097035 @default.
- W3211119963 cites W1966710814 @default.
- W3211119963 cites W1967390332 @default.
- W3211119963 cites W1969016322 @default.
- W3211119963 cites W1987263882 @default.
- W3211119963 cites W2008981917 @default.
- W3211119963 cites W2014612117 @default.
- W3211119963 cites W2018195496 @default.
- W3211119963 cites W2018499562 @default.
- W3211119963 cites W2027181922 @default.
- W3211119963 cites W2028081771 @default.
- W3211119963 cites W2038785867 @default.
- W3211119963 cites W2054479507 @default.
- W3211119963 cites W2073308013 @default.
- W3211119963 cites W2076673261 @default.
- W3211119963 cites W2079674497 @default.
- W3211119963 cites W2084866431 @default.
- W3211119963 cites W2253211496 @default.
- W3211119963 cites W2287024948 @default.
- W3211119963 cites W2502022499 @default.
- W3211119963 cites W2570115779 @default.
- W3211119963 cites W2591055038 @default.
- W3211119963 cites W2596673522 @default.
- W3211119963 cites W2599137200 @default.
- W3211119963 cites W2604224052 @default.
- W3211119963 cites W2609536029 @default.
- W3211119963 cites W2619163351 @default.
- W3211119963 cites W2753046698 @default.
- W3211119963 cites W2769653311 @default.
- W3211119963 cites W2773098506 @default.
- W3211119963 cites W2784039444 @default.
- W3211119963 cites W2800878814 @default.
- W3211119963 cites W2810830997 @default.
- W3211119963 cites W2822833971 @default.
- W3211119963 cites W2897310878 @default.
- W3211119963 cites W2898328160 @default.
- W3211119963 cites W2901221225 @default.
- W3211119963 cites W2933032303 @default.
- W3211119963 cites W2944033430 @default.
- W3211119963 cites W2950787282 @default.
- W3211119963 cites W2950947237 @default.
- W3211119963 cites W2961808126 @default.
- W3211119963 cites W2961996978 @default.
- W3211119963 cites W2980143432 @default.
- W3211119963 cites W2981527560 @default.
- W3211119963 cites W2983871692 @default.
- W3211119963 cites W2996906097 @default.
- W3211119963 cites W3002822343 @default.
- W3211119963 cites W3015195321 @default.
- W3211119963 cites W3016115181 @default.
- W3211119963 cites W3033215614 @default.
- W3211119963 cites W3033394543 @default.
- W3211119963 cites W3042539004 @default.
- W3211119963 cites W3081471891 @default.
- W3211119963 cites W3089077626 @default.
- W3211119963 cites W3092278321 @default.
- W3211119963 cites W3093853111 @default.
- W3211119963 cites W3097825580 @default.
- W3211119963 cites W3133805736 @default.
- W3211119963 cites W3152902336 @default.
- W3211119963 cites W3042720464 @default.
- W3211119963 doi "https://doi.org/10.1016/j.petsci.2021.10.017" @default.
- W3211119963 hasPublicationYear "2022" @default.
- W3211119963 type Work @default.
- W3211119963 sameAs 3211119963 @default.
- W3211119963 citedByCount "16" @default.
- W3211119963 countsByYear W32111199632022 @default.
- W3211119963 countsByYear W32111199632023 @default.
- W3211119963 crossrefType "journal-article" @default.
- W3211119963 hasAuthorship W3211119963A5002273544 @default.
- W3211119963 hasAuthorship W3211119963A5011560454 @default.
- W3211119963 hasAuthorship W3211119963A5012411460 @default.
- W3211119963 hasAuthorship W3211119963A5041989475 @default.
- W3211119963 hasAuthorship W3211119963A5069168874 @default.
- W3211119963 hasAuthorship W3211119963A5076757967 @default.
- W3211119963 hasAuthorship W3211119963A5079732143 @default.
- W3211119963 hasBestOaLocation W32111199631 @default.
- W3211119963 hasConcept C121332964 @default.
- W3211119963 hasConcept C127313418 @default.
- W3211119963 hasConcept C144027150 @default.
- W3211119963 hasConcept C151730666 @default.
- W3211119963 hasConcept C155954305 @default.
- W3211119963 hasConcept C17409809 @default.
- W3211119963 hasConcept C191897082 @default.
- W3211119963 hasConcept C192562407 @default.