FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1990330246> ?p ?o ?g. }

• W1990330246 endingPage "68" @default.
• W1990330246 startingPage "48" @default.
• W1990330246 abstract "The Upper Cretaceous Mesaverde Group in the Piceance Basin, western Colorado, contains thick sections of low porosity, low permeability sandstones that are reservoirs for large accumulations of hydrocarbon gas. The Mesaverde sandstones are lithic arkoses and feldspathic litharenites, containing quartz, plagioclase, variable K-feldspar, chert, and volcanic rock fragments. Important diagenetic processes that have affected the sandstones include compaction, dissolution of feldspar and/or alteration to clay, precipitation of carbonate and quartz cements, precipitation of illite, and alteration of detrital clays (mixed-layer illite–smectite). Porosity is relatively constant; a decrease in primary porosity downward is approximately balanced by an increase in secondary porosity, with significant microporosity in authigenic and diagenetic clays. K-feldspar is almost completely absent below 5500 feet (1675 m). Fibrous illite is relatively abundant above this depth and variable in abundance below. The K–Ar ages of the clays increase with depth, from 40 m.y. at the top of the sampled section to 55 m.y. at the base, indicating illitization of a precursor smectite at approximately the 100 °C isotherm. Samples with abundant fibrous illite have relatively smaller age values. Mass balance calculations indicate that dissolution of K-feldspar, illitization of smectite and precipitation of fibrous illite were coupled. These reactions suggest the transport of dissolved potassium upward hundreds of feet (100–300 m) in the section, possibly associated with water driven vertically by the migration of gas." @default.
• W1990330246 created "2016-06-24" @default.
• W1990330246 creator A5022560291 @default.
• W1990330246 creator A5042742215 @default.
• W1990330246 creator A5064199623 @default.
• W1990330246 creator A5075700268 @default.
• W1990330246 date "2013-02-01" @default.
• W1990330246 modified "2023-10-01" @default.
• W1990330246 title "Diagenesis of a tight gas sand reservoir: Upper Cretaceous Mesaverde Group, Piceance Basin, Colorado" @default.
• W1990330246 cites W1258621943 @default.
• W1990330246 cites W1831255565 @default.
• W1990330246 cites W1879312791 @default.
• W1990330246 cites W1954664792 @default.
• W1990330246 cites W1975247751 @default.
• W1990330246 cites W2004380594 @default.
• W1990330246 cites W2009193496 @default.
• W1990330246 cites W2011963573 @default.
• W1990330246 cites W2023135402 @default.
• W1990330246 cites W2027418634 @default.
• W1990330246 cites W2031236971 @default.
• W1990330246 cites W2031255046 @default.
• W1990330246 cites W2034744635 @default.
• W1990330246 cites W2052433096 @default.
• W1990330246 cites W2052694638 @default.
• W1990330246 cites W2075542607 @default.
• W1990330246 cites W2083440302 @default.
• W1990330246 cites W2086219192 @default.
• W1990330246 cites W2094290315 @default.
• W1990330246 cites W2098476342 @default.
• W1990330246 cites W2108192748 @default.
• W1990330246 cites W2128118921 @default.
• W1990330246 cites W2132362356 @default.
• W1990330246 cites W2143453653 @default.
• W1990330246 cites W2145604970 @default.
• W1990330246 cites W2147152564 @default.
• W1990330246 cites W2155405934 @default.
• W1990330246 cites W2156373425 @default.
• W1990330246 cites W2161130424 @default.
• W1990330246 cites W2162910251 @default.
• W1990330246 cites W2164663173 @default.
• W1990330246 cites W2270535396 @default.
• W1990330246 cites W2339772170 @default.
• W1990330246 cites W4254897223 @default.
• W1990330246 doi "https://doi.org/10.1016/j.marpetgeo.2012.08.003" @default.
• W1990330246 hasPublicationYear "2013" @default.
• W1990330246 type Work @default.
• W1990330246 sameAs 1990330246 @default.
• W1990330246 citedByCount "115" @default.
• W1990330246 countsByYear W19903302462014 @default.
• W1990330246 countsByYear W19903302462015 @default.
• W1990330246 countsByYear W19903302462016 @default.
• W1990330246 countsByYear W19903302462017 @default.
• W1990330246 countsByYear W19903302462018 @default.
• W1990330246 countsByYear W19903302462019 @default.
• W1990330246 countsByYear W19903302462020 @default.
• W1990330246 countsByYear W19903302462021 @default.
• W1990330246 countsByYear W19903302462022 @default.
• W1990330246 countsByYear W19903302462023 @default.
• W1990330246 crossrefType "journal-article" @default.
• W1990330246 hasAuthorship W1990330246A5022560291 @default.
• W1990330246 hasAuthorship W1990330246A5042742215 @default.
• W1990330246 hasAuthorship W1990330246A5064199623 @default.
• W1990330246 hasAuthorship W1990330246A5075700268 @default.
• W1990330246 hasConcept C115393850 @default.
• W1990330246 hasConcept C127313418 @default.
• W1990330246 hasConcept C130452526 @default.
• W1990330246 hasConcept C138170599 @default.
• W1990330246 hasConcept C151730666 @default.
• W1990330246 hasConcept C17409809 @default.
• W1990330246 hasConcept C199289684 @default.
• W1990330246 hasConcept C2778520076 @default.
• W1990330246 hasConcept C2779429093 @default.
• W1990330246 hasConcept C2779870107 @default.
• W1990330246 hasConcept C40212044 @default.
• W1990330246 hasConcept C6494504 @default.
• W1990330246 hasConceptScore W1990330246C115393850 @default.
• W1990330246 hasConceptScore W1990330246C127313418 @default.
• W1990330246 hasConceptScore W1990330246C130452526 @default.
• W1990330246 hasConceptScore W1990330246C138170599 @default.
• W1990330246 hasConceptScore W1990330246C151730666 @default.
• W1990330246 hasConceptScore W1990330246C17409809 @default.
• W1990330246 hasConceptScore W1990330246C199289684 @default.
• W1990330246 hasConceptScore W1990330246C2778520076 @default.
• W1990330246 hasConceptScore W1990330246C2779429093 @default.
• W1990330246 hasConceptScore W1990330246C2779870107 @default.
• W1990330246 hasConceptScore W1990330246C40212044 @default.
• W1990330246 hasConceptScore W1990330246C6494504 @default.
• W1990330246 hasLocation W19903302461 @default.
• W1990330246 hasOpenAccess W1990330246 @default.
• W1990330246 hasPrimaryLocation W19903302461 @default.
• W1990330246 hasRelatedWork W1590341667 @default.
• W1990330246 hasRelatedWork W1956816727 @default.
• W1990330246 hasRelatedWork W1979075196 @default.
• W1990330246 hasRelatedWork W2065101391 @default.
• W1990330246 hasRelatedWork W2086541084 @default.
• W1990330246 hasRelatedWork W2143453653 @default.
• W1990330246 hasRelatedWork W2166316214 @default.
• W1990330246 hasRelatedWork W2381937447 @default.

• next