FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2783016334> ?p ?o ?g. }

• W2783016334 endingPage "182" @default.
• W2783016334 startingPage "166" @default.
• W2783016334 abstract "Abstract Understanding microbial carbonate is one of the most challenging issues in the field of carbonate sedimentology and reservoir. The biotic and abiotic processes that control microbial carbonate precipitation are becoming more established, but the influence of subsequent diagenesis on microbial carbonate reservoirs has not been adequately studied. Here, we describe microbial carbonate from the lower Cambrian Qingxudong Formation in southeastern Sichuan Basin to assess their formation, textures and subsequent diagenesis. Six stages of calcite cementation (Calcite-1 to Calcite-6) and four stages of dissolution (Dis-1 to Dis-4) were identified in microbialites of the Qingxudong Formation. Stromatolites and thrombolites have a different porosity evolution. Sedimentary processes are the fundamental controlling factors of creating pre-existing pores in stromatolites. For thrombolites, the formation of pre-existing pores is attributed to island dissolution and dolomitization in near-surface processes. Microbial metabolic activities contribute more to the dissolution and dolomitization than mixing water. Meteoric water dissolution (Dis-1) in synsedimentary processes and microbial dissolution (Dis-2) in near-surface processes are the fundamental control factors of porosity creation in microbial carbonate of Qingxudong Formation. Thermochemical sulfate reduction (TSR) is a double-edged sword for the porosity development. The destructive effect of TSR on microbial carbonate reservoirs is greater than the constructive effect. The microbial carbonate reservoirs, especially the fabric-destructive dolomite (Dol-2) evolved by thrombolites, have great potential for gas exploration in the Qingxudong Formation. This study is especially useful for further understanding deeply buried microbialite reservoir formation and development, and deep hydrocarbon exploration in this basin and elsewhere worldwide." @default.
• W2783016334 created "2018-01-26" @default.
• W2783016334 creator A5002711718 @default.
• W2783016334 creator A5010672946 @default.
• W2783016334 creator A5054316800 @default.
• W2783016334 creator A5059872112 @default.
• W2783016334 creator A5078501240 @default.
• W2783016334 creator A5083193780 @default.
• W2783016334 date "2018-03-01" @default.
• W2783016334 modified "2023-10-14" @default.
• W2783016334 title "Diagenesis of microbialites in the lower Cambrian Qingxudong Formation, South China: Implications for the origin of porosity in deep microbial carbonates" @default.
• W2783016334 cites W1876889604 @default.
• W2783016334 cites W1881826630 @default.
• W2783016334 cites W1894837831 @default.
• W2783016334 cites W1931078265 @default.
• W2783016334 cites W1943121318 @default.
• W2783016334 cites W1966571928 @default.
• W2783016334 cites W1967147655 @default.
• W2783016334 cites W1974263712 @default.
• W2783016334 cites W1982569011 @default.
• W2783016334 cites W1984727345 @default.
• W2783016334 cites W1987542207 @default.
• W2783016334 cites W1990154555 @default.
• W2783016334 cites W1991362306 @default.
• W2783016334 cites W1994470258 @default.
• W2783016334 cites W1995313824 @default.
• W2783016334 cites W1998837502 @default.
• W2783016334 cites W1999373172 @default.
• W2783016334 cites W1999711327 @default.
• W2783016334 cites W2005231757 @default.
• W2783016334 cites W2012553399 @default.
• W2783016334 cites W2013336440 @default.
• W2783016334 cites W2013684694 @default.
• W2783016334 cites W2015175020 @default.
• W2783016334 cites W2016656075 @default.
• W2783016334 cites W2022462295 @default.
• W2783016334 cites W2033124940 @default.
• W2783016334 cites W2034212523 @default.
• W2783016334 cites W2035586304 @default.
• W2783016334 cites W2053503670 @default.
• W2783016334 cites W2076731456 @default.
• W2783016334 cites W2077873201 @default.
• W2783016334 cites W2081103198 @default.
• W2783016334 cites W2084940867 @default.
• W2783016334 cites W2086484327 @default.
• W2783016334 cites W2089487085 @default.
• W2783016334 cites W2096522903 @default.
• W2783016334 cites W2107740207 @default.
• W2783016334 cites W2114331236 @default.
• W2783016334 cites W2138298930 @default.
• W2783016334 cites W2150772200 @default.
• W2783016334 cites W2150925076 @default.
• W2783016334 cites W2189694045 @default.
• W2783016334 cites W2290815423 @default.
• W2783016334 cites W2566189412 @default.
• W2783016334 cites W269539919 @default.
• W2783016334 cites W2773339937 @default.
• W2783016334 doi "https://doi.org/10.1016/j.jngse.2017.12.031" @default.
• W2783016334 hasPublicationYear "2018" @default.
• W2783016334 type Work @default.
• W2783016334 sameAs 2783016334 @default.
• W2783016334 citedByCount "3" @default.
• W2783016334 countsByYear W27830163342019 @default.
• W2783016334 countsByYear W27830163342021 @default.
• W2783016334 countsByYear W27830163342022 @default.
• W2783016334 crossrefType "journal-article" @default.
• W2783016334 hasAuthorship W2783016334A5002711718 @default.
• W2783016334 hasAuthorship W2783016334A5010672946 @default.
• W2783016334 hasAuthorship W2783016334A5054316800 @default.
• W2783016334 hasAuthorship W2783016334A5059872112 @default.
• W2783016334 hasAuthorship W2783016334A5078501240 @default.
• W2783016334 hasAuthorship W2783016334A5083193780 @default.
• W2783016334 hasConcept C127313418 @default.
• W2783016334 hasConcept C130452526 @default.
• W2783016334 hasConcept C151730666 @default.
• W2783016334 hasConcept C17409809 @default.
• W2783016334 hasConcept C187320778 @default.
• W2783016334 hasConcept C6648577 @default.
• W2783016334 hasConceptScore W2783016334C127313418 @default.
• W2783016334 hasConceptScore W2783016334C130452526 @default.
• W2783016334 hasConceptScore W2783016334C151730666 @default.
• W2783016334 hasConceptScore W2783016334C17409809 @default.
• W2783016334 hasConceptScore W2783016334C187320778 @default.
• W2783016334 hasConceptScore W2783016334C6648577 @default.
• W2783016334 hasLocation W27830163341 @default.
• W2783016334 hasOpenAccess W2783016334 @default.
• W2783016334 hasPrimaryLocation W27830163341 @default.
• W2783016334 hasRelatedWork W2011558782 @default.
• W2783016334 hasRelatedWork W2047007167 @default.
• W2783016334 hasRelatedWork W2083992834 @default.
• W2783016334 hasRelatedWork W2114285638 @default.
• W2783016334 hasRelatedWork W2157006488 @default.
• W2783016334 hasRelatedWork W2329773070 @default.
• W2783016334 hasRelatedWork W2334514520 @default.
• W2783016334 hasRelatedWork W2368907693 @default.
• W2783016334 hasRelatedWork W2388528426 @default.
• W2783016334 hasRelatedWork W3004706942 @default.
• W2783016334 hasVolume "51" @default.

• next