FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2173707590> ?p ?o ?g. }

• W2173707590 endingPage "2003" @default.
• W2173707590 startingPage "1991" @default.
• W2173707590 abstract "Elliptic borehole breakouts are usually used to determine the orientation of in situ stress in deep sedimentary basins. The long axes of borehole breakouts are generally perpendicular to the maximum horizontal principal compression stress (SHmax). However, the azimuth of borehole breakouts is found perpendicular to the chief strike (but not to SHmax) of natural fractures in tight reservoirs, Anpeng field of Nanxiang Basin, China. Based on the core data and acoustic and resistivity borehole image logs, the natural fractures are intensively striking at east-west orientation where borehole breakouts occurred in north-south. If the borehole breakouts are induced only by in situ stresses surrounding the well and the borehole breakouts are known at north-south, SHmax should be perpendicular at east-west, but according to analyses of the earthquake focal mechanism in circumjacent regions, hydraulic fracturing data, drilling-induced fracture data, and the production performance data, SHmax is in the northeast-southwest direction. This contradiction indicates that the influence of natural fractures may cause a serious deviation of the azimuth of borehole breakouts. Therefore, in this case, it is unreliable to determine the orientation of in situ stress only by borehole breakouts in fractured tight reservoirs. In addition, the main fluid flow direction is not parallel to the dominant natural fracture, which is controlled by in situ stress in tight reservoirs." @default.
• W2173707590 created "2016-06-24" @default.
• W2173707590 creator A5043667217 @default.
• W2173707590 creator A5056292418 @default.
• W2173707590 creator A5058749575 @default.
• W2173707590 creator A5061088824 @default.
• W2173707590 creator A5066050203 @default.
• W2173707590 creator A5075758636 @default.
• W2173707590 date "2015-11-01" @default.
• W2173707590 modified "2023-09-27" @default.
• W2173707590 title "Unreliable determination of in situ stress orientation by borehole breakouts in fractured tight reservoirs: A case study of the upper Eocene Hetaoyuan Formation in the Anpeng field, Nanxiang Basin, China" @default.
• W2173707590 cites W1531353067 @default.
• W2173707590 cites W1596237072 @default.
• W2173707590 cites W1965571614 @default.
• W2173707590 cites W1976980828 @default.
• W2173707590 cites W1979819137 @default.
• W2173707590 cites W1987263882 @default.
• W2173707590 cites W2003776659 @default.
• W2173707590 cites W2006027570 @default.
• W2173707590 cites W2025091235 @default.
• W2173707590 cites W2027891895 @default.
• W2173707590 cites W2035630376 @default.
• W2173707590 cites W2037162846 @default.
• W2173707590 cites W2058871289 @default.
• W2173707590 cites W2068216186 @default.
• W2173707590 cites W2076673261 @default.
• W2173707590 cites W2083678379 @default.
• W2173707590 cites W2091043127 @default.
• W2173707590 cites W2102114010 @default.
• W2173707590 cites W2102137637 @default.
• W2173707590 cites W2126372509 @default.
• W2173707590 cites W2127534363 @default.
• W2173707590 cites W2130312129 @default.
• W2173707590 cites W2132814790 @default.
• W2173707590 cites W2141507751 @default.
• W2173707590 cites W2143252260 @default.
• W2173707590 cites W217022991 @default.
• W2173707590 cites W2266968534 @default.
• W2173707590 cites W2371261615 @default.
• W2173707590 cites W2377708919 @default.
• W2173707590 cites W2381583552 @default.
• W2173707590 cites W2382500568 @default.
• W2173707590 cites W2384084291 @default.
• W2173707590 cites W2390261469 @default.
• W2173707590 cites W2393108372 @default.
• W2173707590 cites W2626837308 @default.
• W2173707590 doi "https://doi.org/10.1306/06011513195" @default.
• W2173707590 hasPublicationYear "2015" @default.
• W2173707590 type Work @default.
• W2173707590 sameAs 2173707590 @default.
• W2173707590 citedByCount "9" @default.
• W2173707590 countsByYear W21737075902017 @default.
• W2173707590 countsByYear W21737075902018 @default.
• W2173707590 countsByYear W21737075902019 @default.
• W2173707590 countsByYear W21737075902020 @default.
• W2173707590 countsByYear W21737075902022 @default.
• W2173707590 countsByYear W21737075902023 @default.
• W2173707590 crossrefType "journal-article" @default.
• W2173707590 hasAuthorship W2173707590A5043667217 @default.
• W2173707590 hasAuthorship W2173707590A5056292418 @default.
• W2173707590 hasAuthorship W2173707590A5058749575 @default.
• W2173707590 hasAuthorship W2173707590A5061088824 @default.
• W2173707590 hasAuthorship W2173707590A5066050203 @default.
• W2173707590 hasAuthorship W2173707590A5075758636 @default.
• W2173707590 hasConcept C109007969 @default.
• W2173707590 hasConcept C121332964 @default.
• W2173707590 hasConcept C127313418 @default.
• W2173707590 hasConcept C135628077 @default.
• W2173707590 hasConcept C138885662 @default.
• W2173707590 hasConcept C150560799 @default.
• W2173707590 hasConcept C151730666 @default.
• W2173707590 hasConcept C165205528 @default.
• W2173707590 hasConcept C166957645 @default.
• W2173707590 hasConcept C191935318 @default.
• W2173707590 hasConcept C21036866 @default.
• W2173707590 hasConcept C2778414698 @default.
• W2173707590 hasConcept C41895202 @default.
• W2173707590 hasConcept C95457728 @default.
• W2173707590 hasConcept C97355855 @default.
• W2173707590 hasConceptScore W2173707590C109007969 @default.
• W2173707590 hasConceptScore W2173707590C121332964 @default.
• W2173707590 hasConceptScore W2173707590C127313418 @default.
• W2173707590 hasConceptScore W2173707590C135628077 @default.
• W2173707590 hasConceptScore W2173707590C138885662 @default.
• W2173707590 hasConceptScore W2173707590C150560799 @default.
• W2173707590 hasConceptScore W2173707590C151730666 @default.
• W2173707590 hasConceptScore W2173707590C165205528 @default.
• W2173707590 hasConceptScore W2173707590C166957645 @default.
• W2173707590 hasConceptScore W2173707590C191935318 @default.
• W2173707590 hasConceptScore W2173707590C21036866 @default.
• W2173707590 hasConceptScore W2173707590C2778414698 @default.
• W2173707590 hasConceptScore W2173707590C41895202 @default.
• W2173707590 hasConceptScore W2173707590C95457728 @default.
• W2173707590 hasConceptScore W2173707590C97355855 @default.
• W2173707590 hasIssue "11" @default.
• W2173707590 hasLocation W21737075901 @default.
• W2173707590 hasOpenAccess W2173707590 @default.
• W2173707590 hasPrimaryLocation W21737075901 @default.

• next