FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2099381636> ?p ?o ?g. }

• W2099381636 abstract "Calcite cement derived intraformationally in seven stratigraphic units of marine origin (five submarine-fan deposits and two shelf deposits) is distributed heterogeneously at the outcrop scale. Sandstone beds intercalated with calcareous shale older than Pliocene tend to be completely cemented, whereas stacked sandstone beds that lack shale interbeds have calcite cement in the form of tightly cemented concretions that make up only 10-30% of a bed. The abundance and distribution of concretions, with few exceptions, are irregular and unpredictable. Concretion shapes include spheres (<1 m diameter), oblate and prolate spheroids (<1.5 m), tabular forms (to 8 m long), and irregular forms. Patterns of concretions within beds are remarkably varied and include both random and uniform spacing; preference for either the top, middle, or bottom of beds; preference for faults that cut bedding at a high angle; and localization around shale rip-up clasts. There is no preference of concretions for shell-rich layers. Some formations have cement patterns specific to that formation, whereas other formations have different patterns at different outcrops. Most formations have more than one cement pattern in an outcrop. The lack of strong textural (grain size, graded bedding) or compositional controls on the localization of calcite cement suggests the preeminence of highly localized hydrologic factors in determining the spatial distribution of authigenic pore-filling calcite. Spherical concretions grew by diffusive supply of intraformationally derived components, whereas prolate and elongate concretions grew chiefly under the influence of advective supply. Faults apparently served as fluid conduits and were selectively cemented. In general, only sandstones intercalated with shale are totally cemented. This indicates that shales were a major source of cement components for these sandstones at least." @default.
• W2099381636 created "2016-06-24" @default.
• W2099381636 creator A5001252862 @default.
• W2099381636 date "1995-01-01" @default.
• W2099381636 modified "2023-09-26" @default.
• W2099381636 title "Heterogeneous Distribution of Calcite Cement at the Outcrop Scale in Tertiary Sandstones, Northern Apennines, Italy" @default.
• W2099381636 cites W132106993 @default.
• W2099381636 cites W1525438857 @default.
• W2099381636 cites W1969484087 @default.
• W2099381636 cites W1975482605 @default.
• W2099381636 cites W1976639625 @default.
• W2099381636 cites W1986411002 @default.
• W2099381636 cites W1992259825 @default.
• W2099381636 cites W1998463507 @default.
• W2099381636 cites W1999989851 @default.
• W2099381636 cites W2001817815 @default.
• W2099381636 cites W2011307050 @default.
• W2099381636 cites W2015994472 @default.
• W2099381636 cites W2022739453 @default.
• W2099381636 cites W2044237274 @default.
• W2099381636 cites W2044477877 @default.
• W2099381636 cites W2047533256 @default.
• W2099381636 cites W2067981048 @default.
• W2099381636 cites W2070957121 @default.
• W2099381636 cites W2077821547 @default.
• W2099381636 cites W2079367175 @default.
• W2099381636 cites W2081999568 @default.
• W2099381636 cites W2086234625 @default.
• W2099381636 cites W2086919066 @default.
• W2099381636 cites W2093322180 @default.
• W2099381636 cites W2103381555 @default.
• W2099381636 cites W2103816821 @default.
• W2099381636 cites W2106890627 @default.
• W2099381636 cites W2112061449 @default.
• W2099381636 cites W2118500626 @default.
• W2099381636 cites W2126347921 @default.
• W2099381636 cites W2129657746 @default.
• W2099381636 cites W2141670849 @default.
• W2099381636 cites W2147819868 @default.
• W2099381636 cites W2151293842 @default.
• W2099381636 cites W2156315628 @default.
• W2099381636 cites W2160809941 @default.
• W2099381636 cites W2161097624 @default.
• W2099381636 cites W2165598399 @default.
• W2099381636 cites W2254317040 @default.
• W2099381636 cites W2324831244 @default.
• W2099381636 cites W2520628348 @default.
• W2099381636 cites W2900164201 @default.
• W2099381636 cites W2912130526 @default.
• W2099381636 cites W2965477782 @default.
• W2099381636 cites W3143823162 @default.
• W2099381636 cites W3149161268 @default.
• W2099381636 doi "https://doi.org/10.1306/8d2b21c3-171e-11d7-8645000102c1865d" @default.
• W2099381636 hasPublicationYear "1995" @default.
• W2099381636 type Work @default.
• W2099381636 sameAs 2099381636 @default.
• W2099381636 citedByCount "15" @default.
• W2099381636 countsByYear W20993816362012 @default.
• W2099381636 countsByYear W20993816362019 @default.
• W2099381636 countsByYear W20993816362020 @default.
• W2099381636 countsByYear W20993816362023 @default.
• W2099381636 crossrefType "journal-article" @default.
• W2099381636 hasAuthorship W2099381636A5001252862 @default.
• W2099381636 hasConcept C114793014 @default.
• W2099381636 hasConcept C127313418 @default.
• W2099381636 hasConcept C16674752 @default.
• W2099381636 hasConcept C169212394 @default.
• W2099381636 hasConcept C17409809 @default.
• W2099381636 hasConcept C205649164 @default.
• W2099381636 hasConcept C2778755073 @default.
• W2099381636 hasConcept C2780191791 @default.
• W2099381636 hasConcept C58640448 @default.
• W2099381636 hasConceptScore W2099381636C114793014 @default.
• W2099381636 hasConceptScore W2099381636C127313418 @default.
• W2099381636 hasConceptScore W2099381636C16674752 @default.
• W2099381636 hasConceptScore W2099381636C169212394 @default.
• W2099381636 hasConceptScore W2099381636C17409809 @default.
• W2099381636 hasConceptScore W2099381636C205649164 @default.
• W2099381636 hasConceptScore W2099381636C2778755073 @default.
• W2099381636 hasConceptScore W2099381636C2780191791 @default.
• W2099381636 hasConceptScore W2099381636C58640448 @default.
• W2099381636 hasLocation W20993816361 @default.
• W2099381636 hasOpenAccess W2099381636 @default.
• W2099381636 hasPrimaryLocation W20993816361 @default.
• W2099381636 hasRelatedWork W1975776582 @default.
• W2099381636 hasRelatedWork W2086516461 @default.
• W2099381636 hasRelatedWork W2101207025 @default.
• W2099381636 hasRelatedWork W2146831427 @default.
• W2099381636 hasRelatedWork W2325465340 @default.
• W2099381636 hasRelatedWork W2328136399 @default.
• W2099381636 hasRelatedWork W2340564994 @default.
• W2099381636 hasRelatedWork W2347664876 @default.
• W2099381636 hasRelatedWork W2382915239 @default.
• W2099381636 hasRelatedWork W2589079304 @default.
• W2099381636 hasVolume "79" @default.
• W2099381636 isParatext "false" @default.
• W2099381636 isRetracted "false" @default.
• W2099381636 magId "2099381636" @default.
• W2099381636 workType "article" @default.