FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4386575067> ?p ?o ?g. }

• W4386575067 endingPage "105046" @default.
• W4386575067 startingPage "105046" @default.
• W4386575067 abstract "Ooids are a critical yet enigmatic carbonate grains in the geological record. Previous studies have focused their efforts on studying the mode of ooid formation throughout the Phanerozoic via experimental, numerical simulations, and field studies. To date, however, there is little discussion around factors governing the texture, mineralogy, structure, size, and geometry of Cenozoic ooids, particularly in Saudi Arabia. The present article aims to provide insights on key factors controlling the differential growth of Cenozoic ooids in Saudi Arabia by comparing two contrasting carbonate environments and tectonic settings. Here, we studied the Holocene (0.4–2 kya) ooids developed in the tidally dominated carbonate ramp of the Arabian Gulf under a passive margin setting and the Miocene (15–21 mya) ooids from the Red Sea that were developed in a tectonically active, wave-dominated fault-bounded carbonate platform. The Holocene ooids were characterized by aragonitic, heavily micritized and small (max:550 μm) ooids with bioclast-dominated nuclei. In contrast, the Miocene ooids were replaced by dolomite, larger in size (max:820 μm) and significantly less micritized with variable nuclei compositions, such as rock fragments and bioclasts. The variation in the intensity of bioerosion and micritization suggest the Miocene ooids experienced lesser resting stage time than the Holocene ooids developed under the tide regime due to active wave actions. In addition, the Miocene ooids were developed in a fault-bounded margin allowing a higher carbonate saturation state to concentrate in that zone while the Holocene ooids were developed under a widespread distribution of carbonate saturation state in a vast carbonate ramp setting. These findings indicate that original platform geometry and depositional system (tide-vs wave-dominated) are substantial in dictating the duration of ooid resting stage and distribution of carbonate saturation state across the platforms. All these combined, allows the Miocene ooids to grow larger and reaching its equilibrium size faster. This study highlights the importance of coupling platform architecture and other key environmental parameters (wave actions, sediment supply, and tectonic activities) in understanding the formation of Cenozoic ooids." @default.
• W4386575067 created "2023-09-10" @default.
• W4386575067 creator A5051302005 @default.
• W4386575067 creator A5059881838 @default.
• W4386575067 creator A5085007251 @default.
• W4386575067 creator A5092833379 @default.
• W4386575067 date "2023-11-01" @default.
• W4386575067 modified "2023-10-10" @default.
• W4386575067 title "A tale of two Arabian Cenozoic ooids: Factors controlling the differential growth of ooids across the Arabian Plate" @default.
• W4386575067 cites W1531273367 @default.
• W4386575067 cites W1571804710 @default.
• W4386575067 cites W1821990314 @default.
• W4386575067 cites W1973082754 @default.
• W4386575067 cites W1975890505 @default.
• W4386575067 cites W1996133323 @default.
• W4386575067 cites W1997556201 @default.
• W4386575067 cites W1999626549 @default.
• W4386575067 cites W2000298039 @default.
• W4386575067 cites W2007852531 @default.
• W4386575067 cites W2015869431 @default.
• W4386575067 cites W2018779598 @default.
• W4386575067 cites W2021205465 @default.
• W4386575067 cites W2028428194 @default.
• W4386575067 cites W2037428114 @default.
• W4386575067 cites W2041653864 @default.
• W4386575067 cites W2054407275 @default.
• W4386575067 cites W2067688778 @default.
• W4386575067 cites W2071160900 @default.
• W4386575067 cites W2074565145 @default.
• W4386575067 cites W2085992989 @default.
• W4386575067 cites W2115208265 @default.
• W4386575067 cites W2121764137 @default.
• W4386575067 cites W2139361238 @default.
• W4386575067 cites W2144203676 @default.
• W4386575067 cites W2147427800 @default.
• W4386575067 cites W2154294813 @default.
• W4386575067 cites W2156981346 @default.
• W4386575067 cites W2159416131 @default.
• W4386575067 cites W2160055810 @default.
• W4386575067 cites W2217301490 @default.
• W4386575067 cites W2224953029 @default.
• W4386575067 cites W2331842229 @default.
• W4386575067 cites W2474261184 @default.
• W4386575067 cites W2606911636 @default.
• W4386575067 cites W2624976394 @default.
• W4386575067 cites W2753284915 @default.
• W4386575067 cites W2766659608 @default.
• W4386575067 cites W2767810597 @default.
• W4386575067 cites W2797578994 @default.
• W4386575067 cites W2883066342 @default.
• W4386575067 cites W2886599730 @default.
• W4386575067 cites W2908217770 @default.
• W4386575067 cites W2932696668 @default.
• W4386575067 cites W2950011432 @default.
• W4386575067 cites W2953149450 @default.
• W4386575067 cites W2962883100 @default.
• W4386575067 cites W2973127997 @default.
• W4386575067 cites W3014355492 @default.
• W4386575067 cites W3089120267 @default.
• W4386575067 cites W3123652700 @default.
• W4386575067 cites W3196722247 @default.
• W4386575067 cites W4224245468 @default.
• W4386575067 cites W4292403343 @default.
• W4386575067 cites W4309609812 @default.
• W4386575067 doi "https://doi.org/10.1016/j.jafrearsci.2023.105046" @default.
• W4386575067 hasPublicationYear "2023" @default.
• W4386575067 type Work @default.
• W4386575067 citedByCount "0" @default.
• W4386575067 crossrefType "journal-article" @default.
• W4386575067 hasAuthorship W4386575067A5051302005 @default.
• W4386575067 hasAuthorship W4386575067A5059881838 @default.
• W4386575067 hasAuthorship W4386575067A5085007251 @default.
• W4386575067 hasAuthorship W4386575067A5092833379 @default.
• W4386575067 hasConcept C109007969 @default.
• W4386575067 hasConcept C127313418 @default.
• W4386575067 hasConcept C140345934 @default.
• W4386575067 hasConcept C146588470 @default.
• W4386575067 hasConcept C151730666 @default.
• W4386575067 hasConcept C167570900 @default.
• W4386575067 hasConcept C191897082 @default.
• W4386575067 hasConcept C192562407 @default.
• W4386575067 hasConcept C2778609275 @default.
• W4386575067 hasConcept C2780659211 @default.
• W4386575067 hasConcept C2781471533 @default.
• W4386575067 hasConcept C73707237 @default.
• W4386575067 hasConceptScore W4386575067C109007969 @default.
• W4386575067 hasConceptScore W4386575067C127313418 @default.
• W4386575067 hasConceptScore W4386575067C140345934 @default.
• W4386575067 hasConceptScore W4386575067C146588470 @default.
• W4386575067 hasConceptScore W4386575067C151730666 @default.
• W4386575067 hasConceptScore W4386575067C167570900 @default.
• W4386575067 hasConceptScore W4386575067C191897082 @default.
• W4386575067 hasConceptScore W4386575067C192562407 @default.
• W4386575067 hasConceptScore W4386575067C2778609275 @default.
• W4386575067 hasConceptScore W4386575067C2780659211 @default.
• W4386575067 hasConceptScore W4386575067C2781471533 @default.
• W4386575067 hasConceptScore W4386575067C73707237 @default.
• W4386575067 hasLocation W43865750671 @default.

• next