FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2140147987> ?p ?o ?g. }

• W2140147987 abstract "Paleocave systems form an important class of carbonate reservoirs that are products of near-surface karst processes and later burial compaction and diagenesis. Features and origins of fractures, breccias, and sediment fills associated with paleocave reservoirs have been studied in modern and ancient cave systems. Information about such cave systems is used in this paper to reconstruct the general evolution of paleocave reservoirs and their associated scale, pore networks, and spatial complexities. Spatial complexities in paleocave reservoirs result from near-surface and burial processes. Near-surface processes include dissolutional excavation, clastic sedimentation, chemical precipitation, and localized fracturing, brecciation, and collapse of cave walls and ceilings. Burial processes begin as cave systems subside into the subsurface. Remaining cave passages commonly collapse and early-formed breccia clasts are rebrecciated. Differential compaction of strata around and over collapsed passages produces fractures, crackle breccias, and mosaic breccias. Near-surface and burial processes combine to produce typically complex reservoirs with several scales of heterogeneity. Hydrocarbon reservoirs of paleocave origin are commonly the product of coalesced collapsed-paleocave systems. The coalescing of passages in a cave system into larger, connected porosity zones results from a combination of multiple, cave-forming episodes at composite unconformities and from the collapse of cave systems during burial where surrounding host strata are brecciated and fractured. This combination of processes creates spatially complex reservoirs that can be hundreds to several thousands of meters across, commonly forming large exploration targets. Final size, pore-network types, and spatial complexities of coalesced collapsed-paleocave systems are products of their evolution from near-surface development through burial into the deeper subsurface. The coalesced collapsed-paleocave reservoir hypothesis explains the scale of reservoirs observed and the spatial complexities involved." @default.
• W2140147987 created "2016-06-24" @default.
• W2140147987 creator A5051823166 @default.
• W2140147987 date "1999-01-01" @default.
• W2140147987 modified "2023-10-18" @default.
• W2140147987 title "Paleocave Carbonate Reservoirs: Origins, Burial-Depth Modifications, Spatial Complexity, and Reservoir Implications" @default.
• W2140147987 cites W111886528 @default.
• W2140147987 cites W1500953714 @default.
• W2140147987 cites W15021744 @default.
• W2140147987 cites W1514155192 @default.
• W2140147987 cites W1530554131 @default.
• W2140147987 cites W1604043452 @default.
• W2140147987 cites W1604789055 @default.
• W2140147987 cites W1706632392 @default.
• W2140147987 cites W1769804398 @default.
• W2140147987 cites W1911068942 @default.
• W2140147987 cites W1939198712 @default.
• W2140147987 cites W1954300110 @default.
• W2140147987 cites W1980263581 @default.
• W2140147987 cites W1988382157 @default.
• W2140147987 cites W1993728319 @default.
• W2140147987 cites W1999410840 @default.
• W2140147987 cites W2010011425 @default.
• W2140147987 cites W2010029432 @default.
• W2140147987 cites W2020750452 @default.
• W2140147987 cites W2026844546 @default.
• W2140147987 cites W2052210903 @default.
• W2140147987 cites W2065527413 @default.
• W2140147987 cites W2066344755 @default.
• W2140147987 cites W2096887400 @default.
• W2140147987 cites W2106885242 @default.
• W2140147987 cites W2108340123 @default.
• W2140147987 cites W2118186207 @default.
• W2140147987 cites W2119866941 @default.
• W2140147987 cites W2121639334 @default.
• W2140147987 cites W2125282384 @default.
• W2140147987 cites W2133077874 @default.
• W2140147987 cites W2136812993 @default.
• W2140147987 cites W2147629975 @default.
• W2140147987 cites W2149471565 @default.
• W2140147987 cites W2153676162 @default.
• W2140147987 cites W2231373268 @default.
• W2140147987 cites W2259610414 @default.
• W2140147987 cites W2412699863 @default.
• W2140147987 cites W249371329 @default.
• W2140147987 cites W3125246477 @default.
• W2140147987 cites W48740587 @default.
• W2140147987 cites W579102603 @default.
• W2140147987 doi "https://doi.org/10.1306/e4fd426f-1732-11d7-8645000102c1865d" @default.
• W2140147987 hasPublicationYear "1999" @default.
• W2140147987 type Work @default.
• W2140147987 sameAs 2140147987 @default.
• W2140147987 citedByCount "88" @default.
• W2140147987 countsByYear W21401479872012 @default.
• W2140147987 countsByYear W21401479872013 @default.
• W2140147987 countsByYear W21401479872014 @default.
• W2140147987 countsByYear W21401479872015 @default.
• W2140147987 countsByYear W21401479872016 @default.
• W2140147987 countsByYear W21401479872017 @default.
• W2140147987 countsByYear W21401479872018 @default.
• W2140147987 countsByYear W21401479872019 @default.
• W2140147987 countsByYear W21401479872020 @default.
• W2140147987 countsByYear W21401479872021 @default.
• W2140147987 countsByYear W21401479872022 @default.
• W2140147987 countsByYear W21401479872023 @default.
• W2140147987 crossrefType "journal-article" @default.
• W2140147987 hasAuthorship W2140147987A5051823166 @default.
• W2140147987 hasConcept C127313418 @default.
• W2140147987 hasConcept C16674752 @default.
• W2140147987 hasConcept C17409809 @default.
• W2140147987 hasConcept C191897082 @default.
• W2140147987 hasConcept C192562407 @default.
• W2140147987 hasConcept C2780659211 @default.
• W2140147987 hasConceptScore W2140147987C127313418 @default.
• W2140147987 hasConceptScore W2140147987C16674752 @default.
• W2140147987 hasConceptScore W2140147987C17409809 @default.
• W2140147987 hasConceptScore W2140147987C191897082 @default.
• W2140147987 hasConceptScore W2140147987C192562407 @default.
• W2140147987 hasConceptScore W2140147987C2780659211 @default.
• W2140147987 hasLocation W21401479871 @default.
• W2140147987 hasOpenAccess W2140147987 @default.
• W2140147987 hasPrimaryLocation W21401479871 @default.
• W2140147987 hasRelatedWork W1758497512 @default.
• W2140147987 hasRelatedWork W1987691177 @default.
• W2140147987 hasRelatedWork W2036099453 @default.
• W2140147987 hasRelatedWork W2040829098 @default.
• W2140147987 hasRelatedWork W2124105426 @default.
• W2140147987 hasRelatedWork W2349947565 @default.
• W2140147987 hasRelatedWork W2361911732 @default.
• W2140147987 hasRelatedWork W2538103680 @default.
• W2140147987 hasRelatedWork W3008763070 @default.
• W2140147987 hasRelatedWork W4235203013 @default.
• W2140147987 hasVolume "83" @default.
• W2140147987 isParatext "false" @default.
• W2140147987 isRetracted "false" @default.
• W2140147987 magId "2140147987" @default.
• W2140147987 workType "article" @default.