FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2143262280> ?p ?o ?g. }

• W2143262280 endingPage "885" @default.
• W2143262280 startingPage "873" @default.
• W2143262280 abstract "This study describes porosity reduction by brittle deformation and the application of Touchstone sandstone diagenesis modeling software to assess the relative timing and interactions between grain fracturing and cement formation during burial compaction. Two examples from a previous study of compactional fracturing are used: the Oligocene Frio Formation, Gulf of Mexico Basin, and the Cambrian Mount Simon Formation, Illinois Basin, United States. Grain fracturing during compaction creates intragranular fracture surfaces that are favorable sites for quartz nucleation compared to external grain surfaces that may bear coatings that inhibit the nucleation and growth of quartz cement. Thus, the progress of brittle fracture processes during diagenesis affects quartz cementation. In turn, modeling of the quartz cementation process can serve to place fracturing into its proper context in burial history. In the Mount Simon Formation, the extent of brittle deformation of quartz grains correlates with reconstructed effective stress at the onset of quartz cementation. For Frio Formation samples, however, the extent of brittle deformation does not correlate well with reconstructed effective stress obtained using a one-dimensional basin model that uses compaction disequilibrium as the dominant mechanism for overpressure generation. Judging from the observed degree of grain fracturing, significant fluid overpressures in the Frio may not have developed at the shallow depths indicated by our basin models. The degree of compactional fracturing in sandstones constitutes observable evidence that can be used to decipher the complexities of pressure history." @default.
• W2143262280 created "2016-06-24" @default.
• W2143262280 creator A5006378908 @default.
• W2143262280 creator A5075378150 @default.
• W2143262280 creator A5086373620 @default.
• W2143262280 date "2006-06-01" @default.
• W2143262280 modified "2023-09-27" @default.
• W2143262280 title "Diagenetic modeling to assess the relative timing of quartz cementation and brittle grain processes during compaction" @default.
• W2143262280 cites W1318062 @default.
• W2143262280 cites W1537811147 @default.
• W2143262280 cites W1544422900 @default.
• W2143262280 cites W1545634678 @default.
• W2143262280 cites W1559592307 @default.
• W2143262280 cites W1561579100 @default.
• W2143262280 cites W1846255149 @default.
• W2143262280 cites W1969402793 @default.
• W2143262280 cites W1973027471 @default.
• W2143262280 cites W1987998909 @default.
• W2143262280 cites W1991432315 @default.
• W2143262280 cites W2007434786 @default.
• W2143262280 cites W2019040376 @default.
• W2143262280 cites W2031484793 @default.
• W2143262280 cites W2041668731 @default.
• W2143262280 cites W2050655165 @default.
• W2143262280 cites W2051052126 @default.
• W2143262280 cites W2051363237 @default.
• W2143262280 cites W2053997518 @default.
• W2143262280 cites W2056757731 @default.
• W2143262280 cites W2067261112 @default.
• W2143262280 cites W2069263377 @default.
• W2143262280 cites W2090146652 @default.
• W2143262280 cites W2097247204 @default.
• W2143262280 cites W2099874169 @default.
• W2143262280 cites W2115437113 @default.
• W2143262280 cites W2116130991 @default.
• W2143262280 cites W2119062511 @default.
• W2143262280 cites W2126963790 @default.
• W2143262280 cites W2127664225 @default.
• W2143262280 cites W2139424261 @default.
• W2143262280 cites W2142688952 @default.
• W2143262280 cites W2144944492 @default.
• W2143262280 cites W2146897299 @default.
• W2143262280 cites W2157421823 @default.
• W2143262280 cites W2161960613 @default.
• W2143262280 cites W2166270526 @default.
• W2143262280 cites W2166474285 @default.
• W2143262280 cites W2167385998 @default.
• W2143262280 cites W2201613842 @default.
• W2143262280 cites W2244629780 @default.
• W2143262280 cites W2317582887 @default.
• W2143262280 cites W2320480112 @default.
• W2143262280 cites W2324026987 @default.
• W2143262280 cites W2326636698 @default.
• W2143262280 cites W2343270794 @default.
• W2143262280 cites W2622352898 @default.
• W2143262280 cites W2746321372 @default.
• W2143262280 cites W3127233968 @default.
• W2143262280 cites W3128928778 @default.
• W2143262280 cites W636295422 @default.
• W2143262280 cites W2087098076 @default.
• W2143262280 doi "https://doi.org/10.1306/12190505044" @default.
• W2143262280 hasPublicationYear "2006" @default.
• W2143262280 type Work @default.
• W2143262280 sameAs 2143262280 @default.
• W2143262280 citedByCount "42" @default.
• W2143262280 countsByYear W21432622802012 @default.
• W2143262280 countsByYear W21432622802013 @default.
• W2143262280 countsByYear W21432622802014 @default.
• W2143262280 countsByYear W21432622802016 @default.
• W2143262280 countsByYear W21432622802018 @default.
• W2143262280 countsByYear W21432622802019 @default.
• W2143262280 countsByYear W21432622802020 @default.
• W2143262280 countsByYear W21432622802021 @default.
• W2143262280 countsByYear W21432622802022 @default.
• W2143262280 countsByYear W21432622802023 @default.
• W2143262280 crossrefType "journal-article" @default.
• W2143262280 hasAuthorship W2143262280A5006378908 @default.
• W2143262280 hasAuthorship W2143262280A5075378150 @default.
• W2143262280 hasAuthorship W2143262280A5086373620 @default.
• W2143262280 hasConcept C127313418 @default.
• W2143262280 hasConcept C130452526 @default.
• W2143262280 hasConcept C136478896 @default.
• W2143262280 hasConcept C151730666 @default.
• W2143262280 hasConcept C159985019 @default.
• W2143262280 hasConcept C17409809 @default.
• W2143262280 hasConcept C187320778 @default.
• W2143262280 hasConcept C192562407 @default.
• W2143262280 hasConcept C196715460 @default.
• W2143262280 hasConcept C2779870107 @default.
• W2143262280 hasConcept C523993062 @default.
• W2143262280 hasConcept C5900021 @default.
• W2143262280 hasConcept C94556721 @default.
• W2143262280 hasConceptScore W2143262280C127313418 @default.
• W2143262280 hasConceptScore W2143262280C130452526 @default.
• W2143262280 hasConceptScore W2143262280C136478896 @default.
• W2143262280 hasConceptScore W2143262280C151730666 @default.
• W2143262280 hasConceptScore W2143262280C159985019 @default.
• W2143262280 hasConceptScore W2143262280C17409809 @default.

• next