FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2214677777> ?p ?o ?g. }

• W2214677777 endingPage "291" @default.
• W2214677777 startingPage "282" @default.
• W2214677777 abstract "Rare earth element (REE) concentration and pattern may provide useful information to constrain the source of dolomitizing fluid. However, REE data measured from carbonates might be complicated by diagenetic alterations or clastic components. It is necessary to identify and evaluate such influences before interpreting REE data properly. REE determined in two types of dolostone, including the fine crystalline (D1) and the medium crystalline dolostone (D2), from the Lower Triassic Feixianguan Formation in the Jiannan area display different concentrations and PAAS-normalized patterns. The D1 dolostone that formed by an early near-surface dolomitization has the relatively higher total REE concentrations (ΣREE) and displays near-flat REE patterns similar to that of the PAAS-normalized North American Shale, implying some influences of the clastic components. This is supported by the fact that the D1 has extremely high Fe and Mn contents but dull to no cathodoluminescence. Contrarily, D2 dolostone has lower ΣREE values. Their REE patterns are characteristics of LREE depletion, negative Ce anomalies, and positive La anomalies consistent with the features of the host limestone that yields the seawater-like features. The lack of correlation between dolomite content and their ΣREE, Ce/Ce*, or (Nd/Yb)SN indicates that clastic components are minor and that dolomitization has no or only a minor impact on REE signatures of the precursor limestone. All those suggest that dolomitization associated with D2 was likely associated with seawater-derived fluids. The distinct REE features of the D1 dolostone are mainly attributed to the contamination of the clastic components rather than the indicators of the different dolomitizing fluid, and thereby provided no information on the sources of dolomitizing fluid. Therefore, the degree of contamination should be evaluated before interpreting the REE data properly, especially for dolostones that formed at or near-surface environments." @default.
• W2214677777 created "2016-06-24" @default.
• W2214677777 creator A5001761107 @default.
• W2214677777 creator A5002337174 @default.
• W2214677777 creator A5032715719 @default.
• W2214677777 creator A5071062966 @default.
• W2214677777 date "2016-02-01" @default.
• W2214677777 modified "2023-09-24" @default.
• W2214677777 title "Use of rare earth element geochemistry to constrain the source of dolomitizing fluid for dolomitization of the Lower Triassic Feixianguan Formation, Jiannan area, China" @default.
• W2214677777 cites W1967145808 @default.
• W2214677777 cites W1968486409 @default.
• W2214677777 cites W1979645008 @default.
• W2214677777 cites W1982093108 @default.
• W2214677777 cites W1991730319 @default.
• W2214677777 cites W1998261673 @default.
• W2214677777 cites W1999373172 @default.
• W2214677777 cites W2004604609 @default.
• W2214677777 cites W2004960266 @default.
• W2214677777 cites W2006815492 @default.
• W2214677777 cites W2016379558 @default.
• W2214677777 cites W2034768959 @default.
• W2214677777 cites W2041374973 @default.
• W2214677777 cites W2052309652 @default.
• W2214677777 cites W2059113139 @default.
• W2214677777 cites W2066450007 @default.
• W2214677777 cites W2067174681 @default.
• W2214677777 cites W2071172756 @default.
• W2214677777 cites W2082972472 @default.
• W2214677777 cites W2086543956 @default.
• W2214677777 cites W2087280943 @default.
• W2214677777 cites W2091794361 @default.
• W2214677777 cites W2133403406 @default.
• W2214677777 cites W2150905650 @default.
• W2214677777 cites W2517847674 @default.
• W2214677777 doi "https://doi.org/10.1016/j.petrol.2015.11.037" @default.
• W2214677777 hasPublicationYear "2016" @default.
• W2214677777 type Work @default.
• W2214677777 sameAs 2214677777 @default.
• W2214677777 citedByCount "10" @default.
• W2214677777 countsByYear W22146777772019 @default.
• W2214677777 countsByYear W22146777772020 @default.
• W2214677777 countsByYear W22146777772021 @default.
• W2214677777 countsByYear W22146777772023 @default.
• W2214677777 crossrefType "journal-article" @default.
• W2214677777 hasAuthorship W2214677777A5001761107 @default.
• W2214677777 hasAuthorship W2214677777A5002337174 @default.
• W2214677777 hasAuthorship W2214677777A5032715719 @default.
• W2214677777 hasAuthorship W2214677777A5071062966 @default.
• W2214677777 hasConcept C109007969 @default.
• W2214677777 hasConcept C127313418 @default.
• W2214677777 hasConcept C130452526 @default.
• W2214677777 hasConcept C138170599 @default.
• W2214677777 hasConcept C146588470 @default.
• W2214677777 hasConcept C151730666 @default.
• W2214677777 hasConcept C17409809 @default.
• W2214677777 hasConcept C178790620 @default.
• W2214677777 hasConcept C185592680 @default.
• W2214677777 hasConcept C19320362 @default.
• W2214677777 hasConcept C199289684 @default.
• W2214677777 hasConcept C2777615417 @default.
• W2214677777 hasConcept C2778537970 @default.
• W2214677777 hasConcept C2780181037 @default.
• W2214677777 hasConcept C2780659211 @default.
• W2214677777 hasConcept C2983155866 @default.
• W2214677777 hasConcept C63662990 @default.
• W2214677777 hasConcept C6494504 @default.
• W2214677777 hasConceptScore W2214677777C109007969 @default.
• W2214677777 hasConceptScore W2214677777C127313418 @default.
• W2214677777 hasConceptScore W2214677777C130452526 @default.
• W2214677777 hasConceptScore W2214677777C138170599 @default.
• W2214677777 hasConceptScore W2214677777C146588470 @default.
• W2214677777 hasConceptScore W2214677777C151730666 @default.
• W2214677777 hasConceptScore W2214677777C17409809 @default.
• W2214677777 hasConceptScore W2214677777C178790620 @default.
• W2214677777 hasConceptScore W2214677777C185592680 @default.
• W2214677777 hasConceptScore W2214677777C19320362 @default.
• W2214677777 hasConceptScore W2214677777C199289684 @default.
• W2214677777 hasConceptScore W2214677777C2777615417 @default.
• W2214677777 hasConceptScore W2214677777C2778537970 @default.
• W2214677777 hasConceptScore W2214677777C2780181037 @default.
• W2214677777 hasConceptScore W2214677777C2780659211 @default.
• W2214677777 hasConceptScore W2214677777C2983155866 @default.
• W2214677777 hasConceptScore W2214677777C63662990 @default.
• W2214677777 hasConceptScore W2214677777C6494504 @default.
• W2214677777 hasFunder F4320321001 @default.
• W2214677777 hasFunder F4320321543 @default.
• W2214677777 hasLocation W22146777771 @default.
• W2214677777 hasOpenAccess W2214677777 @default.
• W2214677777 hasPrimaryLocation W22146777771 @default.
• W2214677777 hasRelatedWork W1233342656 @default.
• W2214677777 hasRelatedWork W1570942571 @default.
• W2214677777 hasRelatedWork W2214677777 @default.
• W2214677777 hasRelatedWork W2381423591 @default.
• W2214677777 hasRelatedWork W2479925264 @default.
• W2214677777 hasRelatedWork W3032974216 @default.
• W2214677777 hasRelatedWork W3136940746 @default.
• W2214677777 hasRelatedWork W3192243988 @default.
• W2214677777 hasRelatedWork W4296403670 @default.

• next