FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2568565013> ?p ?o ?g. }

• W2568565013 endingPage "194" @default.
• W2568565013 startingPage "179" @default.
• W2568565013 abstract "This study aims to determine the depositional facies, diagenetic processes and sequence stratigraphic elements of the subsurface carbonate-evaporite succession of the Upper Jurassic (Kimmeridgian-Tithonian) Surmeh Formation of the Salman Oil Field (the Persian Gulf, Iran), in an attempt to explore their impacts on reservoir quality. The Surmeh Formation consists mainly of carbonate rocks, intercalated with evaporite layers. Petrographically, the Surmeh Formation consists of nine microfacies (MF1-MF9). These microfacies are grouped into three facies associations related to three depositional environments (peritidal flat, lagoon and high-energy shoal) sited on the inner part of a homoclinal carbonate ramp. The recorded diagenetic processes include dolomitization, anhydritization, compaction, micritization, neomorphism, dissolution and cementation. Vertical stacking patterns of the studied facies reveal the presence of three third-order depositional sequences, each of which consists of transgressive systems tract (TST) and highstand systems tract (HST). The TSTs comprise intertidal and lagoon facies whereas the HSTs include supratidal and shoal facies.In terms of their impacts on reservoir quality, the shoal facies represent the best reservoir quality, whereas the peritidal and lagoonal facies exhibit moderate to lowest reservoir quality. Also, poikilotopic anhydrite cement played the most significant role in declining the reservoir quality, whereas the widespread dissolution of labile grains and formation of moldic and vuggy pores contributed in enhancing the reservoir quality. In addition, the HSTs have a better reservoir quality than the TSTs. This study represents an approach to use the depositional facies, diagenetic alterations and sequence stratigraphic framework of carbonate –evaporite succession for a more successful reservoir characterization." @default.
• W2568565013 created "2017-01-13" @default.
• W2568565013 creator A5007296695 @default.
• W2568565013 creator A5012243926 @default.
• W2568565013 creator A5019288162 @default.
• W2568565013 creator A5037670462 @default.
• W2568565013 creator A5054274974 @default.
• W2568565013 creator A5080019897 @default.
• W2568565013 date "2017-05-01" @default.
• W2568565013 modified "2023-10-16" @default.
• W2568565013 title "Facies analysis, diagenesis and sequence stratigraphy of the carbonate-evaporite succession of the Upper Jurassic Surmeh Formation: Impacts on reservoir quality (Salman Oil Field, Persian Gulf, Iran)" @default.
• W2568565013 cites W1793048796 @default.
• W2568565013 cites W1971347745 @default.
• W2568565013 cites W1972519865 @default.
• W2568565013 cites W1973351339 @default.
• W2568565013 cites W1973978619 @default.
• W2568565013 cites W1997030970 @default.
• W2568565013 cites W1998874188 @default.
• W2568565013 cites W1999626549 @default.
• W2568565013 cites W2003140278 @default.
• W2568565013 cites W2020594208 @default.
• W2568565013 cites W2029640854 @default.
• W2568565013 cites W2035743016 @default.
• W2568565013 cites W2037308018 @default.
• W2568565013 cites W2042894928 @default.
• W2568565013 cites W2044132433 @default.
• W2568565013 cites W2049124719 @default.
• W2568565013 cites W2049545938 @default.
• W2568565013 cites W2052346014 @default.
• W2568565013 cites W2054223043 @default.
• W2568565013 cites W2058884589 @default.
• W2568565013 cites W2060874912 @default.
• W2568565013 cites W2075283909 @default.
• W2568565013 cites W2085856080 @default.
• W2568565013 cites W2094194853 @default.
• W2568565013 cites W2123680436 @default.
• W2568565013 cites W2134454356 @default.
• W2568565013 cites W2136619267 @default.
• W2568565013 cites W2139326036 @default.
• W2568565013 cites W2142006672 @default.
• W2568565013 cites W2143240126 @default.
• W2568565013 cites W2162795874 @default.
• W2568565013 cites W2166209577 @default.
• W2568565013 cites W2212528985 @default.
• W2568565013 cites W2281361496 @default.
• W2568565013 cites W2346162627 @default.
• W2568565013 cites W2464598037 @default.
• W2568565013 cites W2468712231 @default.
• W2568565013 cites W2910362007 @default.
• W2568565013 cites W2981138633 @default.
• W2568565013 cites W2990128836 @default.
• W2568565013 cites W654711263 @default.
• W2568565013 doi "https://doi.org/10.1016/j.jafrearsci.2017.01.005" @default.
• W2568565013 hasPublicationYear "2017" @default.
• W2568565013 type Work @default.
• W2568565013 sameAs 2568565013 @default.
• W2568565013 citedByCount "42" @default.
• W2568565013 countsByYear W25685650132017 @default.
• W2568565013 countsByYear W25685650132018 @default.
• W2568565013 countsByYear W25685650132019 @default.
• W2568565013 countsByYear W25685650132020 @default.
• W2568565013 countsByYear W25685650132021 @default.
• W2568565013 countsByYear W25685650132022 @default.
• W2568565013 countsByYear W25685650132023 @default.
• W2568565013 crossrefType "journal-article" @default.
• W2568565013 hasAuthorship W2568565013A5007296695 @default.
• W2568565013 hasAuthorship W2568565013A5012243926 @default.
• W2568565013 hasAuthorship W2568565013A5019288162 @default.
• W2568565013 hasAuthorship W2568565013A5037670462 @default.
• W2568565013 hasAuthorship W2568565013A5054274974 @default.
• W2568565013 hasAuthorship W2568565013A5080019897 @default.
• W2568565013 hasConcept C109007969 @default.
• W2568565013 hasConcept C109281948 @default.
• W2568565013 hasConcept C127313418 @default.
• W2568565013 hasConcept C130452526 @default.
• W2568565013 hasConcept C138885662 @default.
• W2568565013 hasConcept C146588470 @default.
• W2568565013 hasConcept C150117547 @default.
• W2568565013 hasConcept C151730666 @default.
• W2568565013 hasConcept C17409809 @default.
• W2568565013 hasConcept C18903297 @default.
• W2568565013 hasConcept C191897082 @default.
• W2568565013 hasConcept C192562407 @default.
• W2568565013 hasConcept C2776527531 @default.
• W2568565013 hasConcept C2778112365 @default.
• W2568565013 hasConcept C2780659211 @default.
• W2568565013 hasConcept C34221334 @default.
• W2568565013 hasConcept C41895202 @default.
• W2568565013 hasConcept C42907665 @default.
• W2568565013 hasConcept C54355233 @default.
• W2568565013 hasConcept C5900021 @default.
• W2568565013 hasConcept C6494504 @default.
• W2568565013 hasConcept C77928131 @default.
• W2568565013 hasConcept C86803240 @default.
• W2568565013 hasConceptScore W2568565013C109007969 @default.
• W2568565013 hasConceptScore W2568565013C109281948 @default.
• W2568565013 hasConceptScore W2568565013C127313418 @default.
• W2568565013 hasConceptScore W2568565013C130452526 @default.

• next