FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2024556904> ?p ?o ?g. }

• W2024556904 abstract "The Smackover Formation in central Mississippi is sour gas productive from siliciclastics interbedded with tight carbonates. The sandstones have low reservoir quality (porosity and permeability of 7.0% and 0.35 md, respectively), but wells are capable of producing at high rates and with large volumes because of the extremely large geopressures and locally thick continuous sandstone packages. Production is from a hostile subsurface environment which includes high temperatures (>365{degree}F), high pressures (>0.88 psi/ft), great depths (>20,000 ft), and variable and corrosive sour gas mixtures (CH{sub 4} = 55%, H{sub 2}S = 36%, CO{sub 2} = 9%). Five fields are productive in this trend; Thomasville, the largest field, is used to illustrate the depositional and diagenetic controls on productivity. Deposition occurred as an upward-shoaling sequence of outer ramp to nearshore and sabkha environments. The lower sandstones are bioturbated, low-quality reservoirs interbedded with carbonate mudstones and packstones; the middle interval consists of the thickest and most continuous sandstones that are interpreted to be amalgamated inner-ramp shoal and ridge deposits; the upper interval consists of the common but tight Smackover ooid grainstone shoals that are interbedded with continuous but thin shoal and shoreface sandstone. The middle interval has the best reservoir quality and contains more » 75% of the hydrocarbons. Seismic may be used to map the sandstone packages but not the individual sandstones. In addition to the larger net/gross and more continuous sandstones in the middle zone, two postdepositional controls also govern the reservoir quality. These include small-scale faulting but more importantly diagenetic events which strongly overprint but do not obscure the original depositional control. At least 15 different diagenetic events have occurred in the sour gas fields that have generally decreased reservoir quality. « less" @default.
• W2024556904 created "2016-06-24" @default.
• W2024556904 creator A5081524554 @default.
• W2024556904 date "1990-01-01" @default.
• W2024556904 modified "2023-09-23" @default.
• W2024556904 title "Depositional and Diagenetic Controls on Reservoir Quality and Gas Composition in a Mixed Siliciclastic/Carbonate Setting, Thomasville Field, Mississippi: ABSTRACT" @default.
• W2024556904 doi "https://doi.org/10.1306/44b4bb62-170a-11d7-8645000102c1865d" @default.
• W2024556904 hasPublicationYear "1990" @default.
• W2024556904 type Work @default.
• W2024556904 sameAs 2024556904 @default.
• W2024556904 citedByCount "0" @default.
• W2024556904 crossrefType "journal-article" @default.
• W2024556904 hasAuthorship W2024556904A5081524554 @default.
• W2024556904 hasConcept C109007969 @default.
• W2024556904 hasConcept C113215200 @default.
• W2024556904 hasConcept C113740612 @default.
• W2024556904 hasConcept C114793014 @default.
• W2024556904 hasConcept C116637073 @default.
• W2024556904 hasConcept C126457475 @default.
• W2024556904 hasConcept C126753816 @default.
• W2024556904 hasConcept C127313418 @default.
• W2024556904 hasConcept C130452526 @default.
• W2024556904 hasConcept C133916931 @default.
• W2024556904 hasConcept C146588470 @default.
• W2024556904 hasConcept C151730666 @default.
• W2024556904 hasConcept C17409809 @default.
• W2024556904 hasConcept C178790620 @default.
• W2024556904 hasConcept C185592680 @default.
• W2024556904 hasConcept C186660238 @default.
• W2024556904 hasConcept C191897082 @default.
• W2024556904 hasConcept C192562407 @default.
• W2024556904 hasConcept C19320362 @default.
• W2024556904 hasConcept C2776044767 @default.
• W2024556904 hasConcept C2779229104 @default.
• W2024556904 hasConcept C2780181037 @default.
• W2024556904 hasConcept C2780659211 @default.
• W2024556904 hasConcept C2780886488 @default.
• W2024556904 hasConcept C2781471533 @default.
• W2024556904 hasConcept C34221334 @default.
• W2024556904 hasConcept C5900021 @default.
• W2024556904 hasConcept C59427239 @default.
• W2024556904 hasConcept C63662990 @default.
• W2024556904 hasConcept C6494504 @default.
• W2024556904 hasConcept C77928131 @default.
• W2024556904 hasConcept C83877588 @default.
• W2024556904 hasConcept C93257316 @default.
• W2024556904 hasConceptScore W2024556904C109007969 @default.
• W2024556904 hasConceptScore W2024556904C113215200 @default.
• W2024556904 hasConceptScore W2024556904C113740612 @default.
• W2024556904 hasConceptScore W2024556904C114793014 @default.
• W2024556904 hasConceptScore W2024556904C116637073 @default.
• W2024556904 hasConceptScore W2024556904C126457475 @default.
• W2024556904 hasConceptScore W2024556904C126753816 @default.
• W2024556904 hasConceptScore W2024556904C127313418 @default.
• W2024556904 hasConceptScore W2024556904C130452526 @default.
• W2024556904 hasConceptScore W2024556904C133916931 @default.
• W2024556904 hasConceptScore W2024556904C146588470 @default.
• W2024556904 hasConceptScore W2024556904C151730666 @default.
• W2024556904 hasConceptScore W2024556904C17409809 @default.
• W2024556904 hasConceptScore W2024556904C178790620 @default.
• W2024556904 hasConceptScore W2024556904C185592680 @default.
• W2024556904 hasConceptScore W2024556904C186660238 @default.
• W2024556904 hasConceptScore W2024556904C191897082 @default.
• W2024556904 hasConceptScore W2024556904C192562407 @default.
• W2024556904 hasConceptScore W2024556904C19320362 @default.
• W2024556904 hasConceptScore W2024556904C2776044767 @default.
• W2024556904 hasConceptScore W2024556904C2779229104 @default.
• W2024556904 hasConceptScore W2024556904C2780181037 @default.
• W2024556904 hasConceptScore W2024556904C2780659211 @default.
• W2024556904 hasConceptScore W2024556904C2780886488 @default.
• W2024556904 hasConceptScore W2024556904C2781471533 @default.
• W2024556904 hasConceptScore W2024556904C34221334 @default.
• W2024556904 hasConceptScore W2024556904C5900021 @default.
• W2024556904 hasConceptScore W2024556904C59427239 @default.
• W2024556904 hasConceptScore W2024556904C63662990 @default.
• W2024556904 hasConceptScore W2024556904C6494504 @default.
• W2024556904 hasConceptScore W2024556904C77928131 @default.
• W2024556904 hasConceptScore W2024556904C83877588 @default.
• W2024556904 hasConceptScore W2024556904C93257316 @default.
• W2024556904 hasLocation W20245569041 @default.
• W2024556904 hasOpenAccess W2024556904 @default.
• W2024556904 hasPrimaryLocation W20245569041 @default.
• W2024556904 hasRelatedWork W1524067232 @default.
• W2024556904 hasRelatedWork W1831772678 @default.
• W2024556904 hasRelatedWork W1970487295 @default.
• W2024556904 hasRelatedWork W1990054646 @default.
• W2024556904 hasRelatedWork W2013872005 @default.
• W2024556904 hasRelatedWork W2078870491 @default.
• W2024556904 hasRelatedWork W2094798119 @default.
• W2024556904 hasRelatedWork W2097878964 @default.
• W2024556904 hasRelatedWork W2106136372 @default.
• W2024556904 hasRelatedWork W2109519010 @default.
• W2024556904 hasRelatedWork W2128922390 @default.
• W2024556904 hasRelatedWork W2138455430 @default.
• W2024556904 hasRelatedWork W2253442143 @default.
• W2024556904 hasRelatedWork W2255041356 @default.
• W2024556904 hasRelatedWork W2414567389 @default.
• W2024556904 hasRelatedWork W2578594518 @default.
• W2024556904 hasRelatedWork W2748802752 @default.
• W2024556904 hasRelatedWork W3005925117 @default.

• next