FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2489702557> ?p ?o ?g. }

• W2489702557 endingPage "1164" @default.
• W2489702557 startingPage "1135" @default.
• W2489702557 abstract "The Lower Cretaceous presalt section in the Kwanza Basin contains an excellent petroleum system that includes “synrift” strata (Barremian) overlain by a “sag” interval (Aptian) and capped by the Loeme Salt. The upper synrift is generally limestone with widespread mollusk packstones and grainstones (coquinas) deposited in a fresh-to–moderately saline (alkaline) lake. The sag interval is characterized by carbonate platforms and silica-rich isolated buildups formed in highly evaporated, highly alkaline lakes. Shrubby (dendritic), microbially influenced boundstones and intraclast–spherulite grainstones accumulated in shallow water on platform tops. Microbial cherts were deposited as organic buildups on large, isolated structural highs basinward (west) of platforms, and they apparently formed at low temperatures in very alkaline lake water. Shrubby boundstones and microbial cherts have vuggy pores that are primary and result in high permeability. Wackestones and packstones with calcitic grains (mainly spherulites) in dolomite or argillaceous dolomite were deposited in slightly deeper, low-energy sag environments. In addition, clays (especially stevensite) precipitated out of the silica-rich, highly alkaline lake waters. During sag deposition, calcite precipitated on the shallow lake floor with morphologies that ranged from spherulites to shrubs and included a continuum of intermediate forms. Spherulites probably precipitated just below the sediment–water interface. Spherulites and shrubby calcites are commonly recrystallized. Spherulites floating in stevensite probably formed in deeper lacustrine environments. Organic-rich mudstones were deposited in even deeper lacustrine environments in synrift and sag intervals, and they are likely the source of most hydrocarbons in this system. These interpretations are supported by seismic, core, petrographic, and stable isotope data." @default.
• W2489702557 created "2016-08-23" @default.
• W2489702557 creator A5015475123 @default.
• W2489702557 creator A5045260322 @default.
• W2489702557 creator A5045881916 @default.
• W2489702557 creator A5074230789 @default.
• W2489702557 creator A5077223261 @default.
• W2489702557 creator A5090579606 @default.
• W2489702557 date "2016-07-01" @default.
• W2489702557 modified "2023-10-02" @default.
• W2489702557 title "Presalt stratigraphy and depositional systems in the Kwanza Basin, offshore Angola" @default.
• W2489702557 cites W1521380151 @default.
• W2489702557 cites W1534624437 @default.
• W2489702557 cites W1540990717 @default.
• W2489702557 cites W1547907389 @default.
• W2489702557 cites W1555507629 @default.
• W2489702557 cites W1977829117 @default.
• W2489702557 cites W1982339776 @default.
• W2489702557 cites W1984974891 @default.
• W2489702557 cites W1989270075 @default.
• W2489702557 cites W1990522610 @default.
• W2489702557 cites W1992805349 @default.
• W2489702557 cites W1993898064 @default.
• W2489702557 cites W1994790413 @default.
• W2489702557 cites W2002912225 @default.
• W2489702557 cites W2004850381 @default.
• W2489702557 cites W2005649253 @default.
• W2489702557 cites W2033822779 @default.
• W2489702557 cites W2048163562 @default.
• W2489702557 cites W2052639207 @default.
• W2489702557 cites W2068168634 @default.
• W2489702557 cites W2070603872 @default.
• W2489702557 cites W2080088198 @default.
• W2489702557 cites W2086070119 @default.
• W2489702557 cites W2088385868 @default.
• W2489702557 cites W2092027246 @default.
• W2489702557 cites W2092426793 @default.
• W2489702557 cites W2102899362 @default.
• W2489702557 cites W2105628276 @default.
• W2489702557 cites W2127462477 @default.
• W2489702557 cites W2133223164 @default.
• W2489702557 cites W2139819426 @default.
• W2489702557 cites W2145794341 @default.
• W2489702557 cites W2149388406 @default.
• W2489702557 cites W2160156450 @default.
• W2489702557 cites W2341492403 @default.
• W2489702557 cites W2517847674 @default.
• W2489702557 cites W2741673313 @default.
• W2489702557 cites W590001249 @default.
• W2489702557 cites W89195609 @default.
• W2489702557 doi "https://doi.org/10.1306/02111615216" @default.
• W2489702557 hasPublicationYear "2016" @default.
• W2489702557 type Work @default.
• W2489702557 sameAs 2489702557 @default.
• W2489702557 citedByCount "83" @default.
• W2489702557 countsByYear W24897025572016 @default.
• W2489702557 countsByYear W24897025572017 @default.
• W2489702557 countsByYear W24897025572018 @default.
• W2489702557 countsByYear W24897025572019 @default.
• W2489702557 countsByYear W24897025572020 @default.
• W2489702557 countsByYear W24897025572021 @default.
• W2489702557 countsByYear W24897025572022 @default.
• W2489702557 countsByYear W24897025572023 @default.
• W2489702557 crossrefType "journal-article" @default.
• W2489702557 hasAuthorship W2489702557A5015475123 @default.
• W2489702557 hasAuthorship W2489702557A5045260322 @default.
• W2489702557 hasAuthorship W2489702557A5045881916 @default.
• W2489702557 hasAuthorship W2489702557A5074230789 @default.
• W2489702557 hasAuthorship W2489702557A5077223261 @default.
• W2489702557 hasAuthorship W2489702557A5090579606 @default.
• W2489702557 hasConcept C109007969 @default.
• W2489702557 hasConcept C109281948 @default.
• W2489702557 hasConcept C111368507 @default.
• W2489702557 hasConcept C114793014 @default.
• W2489702557 hasConcept C126753816 @default.
• W2489702557 hasConcept C127313418 @default.
• W2489702557 hasConcept C151730666 @default.
• W2489702557 hasConcept C162284963 @default.
• W2489702557 hasConcept C77928131 @default.
• W2489702557 hasConceptScore W2489702557C109007969 @default.
• W2489702557 hasConceptScore W2489702557C109281948 @default.
• W2489702557 hasConceptScore W2489702557C111368507 @default.
• W2489702557 hasConceptScore W2489702557C114793014 @default.
• W2489702557 hasConceptScore W2489702557C126753816 @default.
• W2489702557 hasConceptScore W2489702557C127313418 @default.
• W2489702557 hasConceptScore W2489702557C151730666 @default.
• W2489702557 hasConceptScore W2489702557C162284963 @default.
• W2489702557 hasConceptScore W2489702557C77928131 @default.
• W2489702557 hasIssue "07" @default.
• W2489702557 hasLocation W24897025571 @default.
• W2489702557 hasOpenAccess W2489702557 @default.
• W2489702557 hasPrimaryLocation W24897025571 @default.
• W2489702557 hasRelatedWork W1937777925 @default.
• W2489702557 hasRelatedWork W2143430481 @default.
• W2489702557 hasRelatedWork W2314000175 @default.
• W2489702557 hasRelatedWork W2324907918 @default.
• W2489702557 hasRelatedWork W2326102876 @default.
• W2489702557 hasRelatedWork W2331057432 @default.

• next