FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3045244932> ?p ?o ?g. }

• W3045244932 endingPage "7997" @default.
• W3045244932 startingPage "7977" @default.
• W3045244932 abstract "Detailed high magnification scanning electron microscopic (SEM) study supported by petrographic, mineralogical, and geochemical (major and trace element) analysis of the Gercus Formation clastics (sandstones and mudstones) from northern Iraq shows that the main authigenic components are carbonate (dolomite and calcite), clay and haematite minerals with rare quartz, feldspar, and gypsum. The carbonates and sulphate minerals were the main early diagenetic phase in the Gercus Formation and were produced from the post‐depositional breakdown of ferromagnesian minerals. These latter are unstable in the oxidizing conditions of the interstitial waters below the desert surface. The main authigenic clay minerals are illite, illite‐smectite, and palygorskite. The presence of tangential illite coating and illite‐smectite in the sandstones can be related to their desert origin. Palygorskite is associated with dolomite, calcite, and haematite. These mineral associations may indicate early diagenesis in evaporitic and saline conditions. It also confirms the syndepositional and diagenetic origin for the clayey‐haematitic matrix and pigment of the Gercus Formation. Haematite occurs as extremely fine‐grained crystals mixed with authigenic clays and exhibits a range of shapes (e.g., fibrous to lath‐shaped aggregates, small spherical grains, specularite crystals, blade‐shaped, rosette‐like clusters, and a lump of bright spheroid‐shaped haematite/goethite). The arid to semi‐arid conditions together with the oxidizing and alkaline interstitial water favoured the noted mineral assemblage within the Gercus Formation." @default.
• W3045244932 created "2020-07-29" @default.
• W3045244932 creator A5027303936 @default.
• W3045244932 creator A5031781879 @default.
• W3045244932 creator A5039293518 @default.
• W3045244932 creator A5074385554 @default.
• W3045244932 date "2020-07-26" @default.
• W3045244932 modified "2023-09-26" @default.
• W3045244932 title "Clay mineral diagenesis and red bed colouration: A<scp>SEM</scp>study of the Gercus Formation (Middle Eocene), northern Iraq" @default.
• W3045244932 cites W1673688546 @default.
• W3045244932 cites W1955254938 @default.
• W3045244932 cites W1968318197 @default.
• W3045244932 cites W1969855377 @default.
• W3045244932 cites W1969925644 @default.
• W3045244932 cites W1973706388 @default.
• W3045244932 cites W1975046382 @default.
• W3045244932 cites W1984130798 @default.
• W3045244932 cites W1988544125 @default.
• W3045244932 cites W1998234041 @default.
• W3045244932 cites W1999136313 @default.
• W3045244932 cites W1999573925 @default.
• W3045244932 cites W2006986578 @default.
• W3045244932 cites W2017310672 @default.
• W3045244932 cites W2022323560 @default.
• W3045244932 cites W2023091835 @default.
• W3045244932 cites W2027646081 @default.
• W3045244932 cites W2031164272 @default.
• W3045244932 cites W2036563260 @default.
• W3045244932 cites W2039172832 @default.
• W3045244932 cites W2055636377 @default.
• W3045244932 cites W2058188237 @default.
• W3045244932 cites W2068960231 @default.
• W3045244932 cites W2085349409 @default.
• W3045244932 cites W2087705600 @default.
• W3045244932 cites W2089119836 @default.
• W3045244932 cites W2099626156 @default.
• W3045244932 cites W2104837834 @default.
• W3045244932 cites W2106229214 @default.
• W3045244932 cites W2109664271 @default.
• W3045244932 cites W2115420813 @default.
• W3045244932 cites W2116969619 @default.
• W3045244932 cites W2135326475 @default.
• W3045244932 cites W2139326036 @default.
• W3045244932 cites W2143735213 @default.
• W3045244932 cites W2153721032 @default.
• W3045244932 cites W2163585364 @default.
• W3045244932 cites W2166993510 @default.
• W3045244932 cites W2168409598 @default.
• W3045244932 cites W2233548737 @default.
• W3045244932 cites W2273039186 @default.
• W3045244932 cites W2533466800 @default.
• W3045244932 cites W2549541397 @default.
• W3045244932 cites W2739516467 @default.
• W3045244932 cites W2752364613 @default.
• W3045244932 cites W2790364767 @default.
• W3045244932 cites W2806350616 @default.
• W3045244932 cites W2926476559 @default.
• W3045244932 cites W2938886180 @default.
• W3045244932 cites W2972249248 @default.
• W3045244932 cites W2983462851 @default.
• W3045244932 cites W4236924214 @default.
• W3045244932 cites W4247165743 @default.
• W3045244932 cites W4255412919 @default.
• W3045244932 cites W4781991 @default.
• W3045244932 cites W4831070 @default.
• W3045244932 doi "https://doi.org/10.1002/gj.3915" @default.
• W3045244932 hasPublicationYear "2020" @default.
• W3045244932 type Work @default.
• W3045244932 sameAs 3045244932 @default.
• W3045244932 citedByCount "4" @default.
• W3045244932 countsByYear W30452449322021 @default.
• W3045244932 countsByYear W30452449322022 @default.
• W3045244932 crossrefType "journal-article" @default.
• W3045244932 hasAuthorship W3045244932A5027303936 @default.
• W3045244932 hasAuthorship W3045244932A5031781879 @default.
• W3045244932 hasAuthorship W3045244932A5039293518 @default.
• W3045244932 hasAuthorship W3045244932A5074385554 @default.
• W3045244932 hasConcept C115393850 @default.
• W3045244932 hasConcept C127313418 @default.
• W3045244932 hasConcept C130452526 @default.
• W3045244932 hasConcept C151730666 @default.
• W3045244932 hasConcept C17409809 @default.
• W3045244932 hasConcept C199289684 @default.
• W3045244932 hasConcept C2776044767 @default.
• W3045244932 hasConcept C2779229104 @default.
• W3045244932 hasConcept C2779429093 @default.
• W3045244932 hasConcept C2780181037 @default.
• W3045244932 hasConcept C2780191791 @default.
• W3045244932 hasConcept C2780873218 @default.
• W3045244932 hasConcept C2781113784 @default.
• W3045244932 hasConcept C40212044 @default.
• W3045244932 hasConcept C59235061 @default.
• W3045244932 hasConceptScore W3045244932C115393850 @default.
• W3045244932 hasConceptScore W3045244932C127313418 @default.
• W3045244932 hasConceptScore W3045244932C130452526 @default.
• W3045244932 hasConceptScore W3045244932C151730666 @default.
• W3045244932 hasConceptScore W3045244932C17409809 @default.
• W3045244932 hasConceptScore W3045244932C199289684 @default.

• next