FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2800490840> ?p ?o ?g. }

• W2800490840 endingPage "1112" @default.
• W2800490840 startingPage "1089" @default.
• W2800490840 abstract "Abstract In 13 years, infrared observations from the Visual and Infrared Mapping Spectrometer onboard Cassini provided significant hints about the spectral and geological diversity of Titan's surface. The analysis of the infrared (IR) signature of spectral units enables constraining the surface composition, which is crucial for understanding possible interactions between Titan's interior, surface, and atmosphere. Here we investigate a selection of areas in the equatorial regions, imaged by Cassini's instruments, which exhibit an apparent transition from the Visual and Infrared Mapping Spectrometer IR‐bright to the IR‐blue and IR‐brown units (from false‐color composites using red: 1.57/1.27 μm, green: 2.01/1.27 μm, and blue: 1.27/1.08 μm). By applying an updated radiative transfer model, we extract the surface albedo of IR units identified in these regions. Then, we compare them with synthetic mixtures of two expected components on Titan's surface, namely, water ice and laboratory tholins. This allows us to reconnect the derived composition and grain size information to the geomorphology observed from Radio Detection and Ranging instrument (RADAR)/Synthetic Aperture Radar images. We interpret IR‐bright units as hills and plains coated by organic material and incised by fluvial networks. Erosion products are transported downstream to areas where IR‐blue units are seen near the IR‐bright units. These units, enriched in water ice, are most likely outwash plains hosting debris from fluvial erosion. Farther away from the IR‐bright units, the IR‐brown units are dominantly made of organics with varied grain sizes, ranging from dust‐ to sand‐sized particles that form the dune fields. The transition areas therefore exhibit trends in water ice content and grain size supported by geomorphological observations." @default.
• W2800490840 created "2018-05-17" @default.
• W2800490840 creator A5001367978 @default.
• W2800490840 creator A5012021226 @default.
• W2800490840 creator A5024210812 @default.
• W2800490840 creator A5035090601 @default.
• W2800490840 creator A5039572579 @default.
• W2800490840 creator A5044560878 @default.
• W2800490840 creator A5045413812 @default.
• W2800490840 creator A5048961733 @default.
• W2800490840 creator A5066286949 @default.
• W2800490840 creator A5069582259 @default.
• W2800490840 creator A5082255494 @default.
• W2800490840 creator A5086243676 @default.
• W2800490840 creator A5086777105 @default.
• W2800490840 date "2018-05-01" @default.
• W2800490840 modified "2023-10-14" @default.
• W2800490840 title "Geological Evolution of Titan's Equatorial Regions: Possible Nature and Origin of the Dune Material" @default.
• W2800490840 cites W1792753740 @default.
• W2800490840 cites W1872718233 @default.
• W2800490840 cites W1903665288 @default.
• W2800490840 cites W1930554885 @default.
• W2800490840 cites W1963557263 @default.
• W2800490840 cites W1968306938 @default.
• W2800490840 cites W1969688604 @default.
• W2800490840 cites W1970430285 @default.
• W2800490840 cites W1973018095 @default.
• W2800490840 cites W1976067301 @default.
• W2800490840 cites W1977107238 @default.
• W2800490840 cites W1978359114 @default.
• W2800490840 cites W1978446652 @default.
• W2800490840 cites W1979197200 @default.
• W2800490840 cites W1979409057 @default.
• W2800490840 cites W1986118217 @default.
• W2800490840 cites W1986241429 @default.
• W2800490840 cites W1987276992 @default.
• W2800490840 cites W1988146940 @default.
• W2800490840 cites W1990737872 @default.
• W2800490840 cites W1991570125 @default.
• W2800490840 cites W1991850349 @default.
• W2800490840 cites W1991862147 @default.
• W2800490840 cites W1993330199 @default.
• W2800490840 cites W1994872271 @default.
• W2800490840 cites W1995973455 @default.
• W2800490840 cites W1997516451 @default.
• W2800490840 cites W1998383233 @default.
• W2800490840 cites W2004694428 @default.
• W2800490840 cites W2007414412 @default.
• W2800490840 cites W2009610229 @default.
• W2800490840 cites W2010146303 @default.
• W2800490840 cites W2012554807 @default.
• W2800490840 cites W2017241437 @default.
• W2800490840 cites W2018714254 @default.
• W2800490840 cites W2019125373 @default.
• W2800490840 cites W2019195466 @default.
• W2800490840 cites W2021066697 @default.
• W2800490840 cites W2022529994 @default.
• W2800490840 cites W2022672094 @default.
• W2800490840 cites W2036413407 @default.
• W2800490840 cites W2038291855 @default.
• W2800490840 cites W2038626884 @default.
• W2800490840 cites W2042750578 @default.
• W2800490840 cites W2045231383 @default.
• W2800490840 cites W2048049407 @default.
• W2800490840 cites W2055440636 @default.
• W2800490840 cites W2058843606 @default.
• W2800490840 cites W2066776950 @default.
• W2800490840 cites W2067127049 @default.
• W2800490840 cites W2071574855 @default.
• W2800490840 cites W2073066914 @default.
• W2800490840 cites W2077866512 @default.
• W2800490840 cites W2080220337 @default.
• W2800490840 cites W2080222835 @default.
• W2800490840 cites W2089384217 @default.
• W2800490840 cites W2089913055 @default.
• W2800490840 cites W2091128659 @default.
• W2800490840 cites W2091505187 @default.
• W2800490840 cites W2092096783 @default.
• W2800490840 cites W2094751488 @default.
• W2800490840 cites W2095517724 @default.
• W2800490840 cites W2104021611 @default.
• W2800490840 cites W2110515514 @default.
• W2800490840 cites W2111560151 @default.
• W2800490840 cites W2115492903 @default.
• W2800490840 cites W2119057720 @default.
• W2800490840 cites W2121797917 @default.
• W2800490840 cites W2121883311 @default.
• W2800490840 cites W2124871727 @default.
• W2800490840 cites W2128062709 @default.
• W2800490840 cites W2128126513 @default.
• W2800490840 cites W2130777744 @default.
• W2800490840 cites W2143373565 @default.
• W2800490840 cites W2145620958 @default.
• W2800490840 cites W2150938638 @default.
• W2800490840 cites W2151385891 @default.
• W2800490840 cites W2174289640 @default.
• W2800490840 cites W2199655957 @default.
• W2800490840 cites W2258812802 @default.

• next