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- W2805528027 abstract "Bakhuysen Crater is a Late Noachian to Early Hesperian age ∼150 km-diameter impact structure located in the heavily cratered southern highlands of Mars. It is one of the largest craters on Mars with well-preserved ejecta deposits. Impact ejecta deposits allow an understanding of crustal composition, volatile content, and evolution of terrestrial planets, yet the emplacement of ejecta deposits on bodies throughout the solar system is still debated. Here, we present the first detailed geomorphologic map of Bakhuysen Crater. We distinguish two distinct ejecta units: (1) a largely hummocky ejecta unit (Be1) that comprises the continuous ejecta blanket; and (2) an uppermost, discontinuous unit (Be2) with a distinct ponded morphology, pitted texture, and previously unreported lobate and flow deposits. Pitted materials are present in the crater interior deposits as well as the ejecta. Bakhuysen is the largest Martian crater thus far identified with crater-related pitted material, which has been suggested previously to represent volatile-rich primary impact melt-bearing deposits. Unit Be1 is interpreted as the continuous ejecta blanket emplaced through ballistic sedimentation and radial flow. Unit Be2 shares many attributes with impact melt-rich ejecta seen on other planetary bodies (e.g., Earth, Moon, and Mercury) and is interpreted as having been emplaced as ground-hugging flows during the later modification stage of crater formation. Channels are observed as having emanated from Bakhuysen impactites and represents a clear example of the role of volatiles in the impact cratering process on Mars. Bakhuysen ejecta deposits and its associated features suggests that, if indeed a substantial volatile source is sampled by Martian impact events, then the formation of ejecta-associated channels on Mars are likely genetically linked to the formation of pitted materials where present. The preservation and exposure of the impact deposits of Bakhuysen present a unique opportunity to study these features and their relationship to the impact process on Mars." @default.
- W2805528027 created "2018-06-13" @default.
- W2805528027 creator A5028438418 @default.
- W2805528027 creator A5047069514 @default.
- W2805528027 creator A5060508061 @default.
- W2805528027 date "2018-11-01" @default.
- W2805528027 modified "2023-09-25" @default.
- W2805528027 title "Ejecta deposits of Bakhuysen Crater, Mars" @default.
- W2805528027 cites W1484635710 @default.
- W2805528027 cites W1525347437 @default.
- W2805528027 cites W1568935506 @default.
- W2805528027 cites W1616140579 @default.
- W2805528027 cites W1634333813 @default.
- W2805528027 cites W1666924183 @default.
- W2805528027 cites W1775723674 @default.
- W2805528027 cites W1874374897 @default.
- W2805528027 cites W1956187030 @default.
- W2805528027 cites W1967113918 @default.
- W2805528027 cites W1968132170 @default.
- W2805528027 cites W1968405878 @default.
- W2805528027 cites W1970748143 @default.
- W2805528027 cites W1971789222 @default.
- W2805528027 cites W1978601643 @default.
- W2805528027 cites W1980729025 @default.
- W2805528027 cites W1980942086 @default.
- W2805528027 cites W1984031617 @default.
- W2805528027 cites W1985206187 @default.
- W2805528027 cites W1986060546 @default.
- W2805528027 cites W1986859129 @default.
- W2805528027 cites W1989363303 @default.
- W2805528027 cites W1992765525 @default.
- W2805528027 cites W1998150091 @default.
- W2805528027 cites W2002137553 @default.
- W2805528027 cites W2002423109 @default.
- W2805528027 cites W2002607051 @default.
- W2805528027 cites W2005701215 @default.
- W2805528027 cites W2009918868 @default.
- W2805528027 cites W2017024114 @default.
- W2805528027 cites W2020615976 @default.
- W2805528027 cites W2021211105 @default.
- W2805528027 cites W2021470802 @default.
- W2805528027 cites W2021722013 @default.
- W2805528027 cites W2026411566 @default.
- W2805528027 cites W2027893742 @default.
- W2805528027 cites W2028483491 @default.
- W2805528027 cites W2028545091 @default.
- W2805528027 cites W2029323704 @default.
- W2805528027 cites W2029515683 @default.
- W2805528027 cites W2034970124 @default.
- W2805528027 cites W2037161682 @default.
- W2805528027 cites W2042371405 @default.
- W2805528027 cites W2043308987 @default.
- W2805528027 cites W2043638143 @default.
- W2805528027 cites W2045323482 @default.
- W2805528027 cites W2046910671 @default.
- W2805528027 cites W2051753189 @default.
- W2805528027 cites W2052402884 @default.
- W2805528027 cites W2060997761 @default.
- W2805528027 cites W2065782610 @default.
- W2805528027 cites W2067594709 @default.
- W2805528027 cites W2076509405 @default.
- W2805528027 cites W2078375547 @default.
- W2805528027 cites W2080969055 @default.
- W2805528027 cites W2081221246 @default.
- W2805528027 cites W2091707644 @default.
- W2805528027 cites W2093918115 @default.
- W2805528027 cites W2094342208 @default.
- W2805528027 cites W2095349867 @default.
- W2805528027 cites W2101283146 @default.
- W2805528027 cites W2102748867 @default.
- W2805528027 cites W2102920959 @default.
- W2805528027 cites W2105801305 @default.
- W2805528027 cites W2107582290 @default.
- W2805528027 cites W2114444450 @default.
- W2805528027 cites W2117586409 @default.
- W2805528027 cites W2118829860 @default.
- W2805528027 cites W2125954106 @default.
- W2805528027 cites W2135277834 @default.
- W2805528027 cites W2137784239 @default.
- W2805528027 cites W2138158236 @default.
- W2805528027 cites W2139733953 @default.
- W2805528027 cites W2140931240 @default.
- W2805528027 cites W2141426107 @default.
- W2805528027 cites W2146376665 @default.
- W2805528027 cites W2147284262 @default.
- W2805528027 cites W2147468238 @default.
- W2805528027 cites W2148965904 @default.
- W2805528027 cites W2162491242 @default.
- W2805528027 cites W2171809264 @default.
- W2805528027 cites W2286050782 @default.
- W2805528027 cites W2552816217 @default.
- W2805528027 cites W2793963985 @default.
- W2805528027 cites W4243063327 @default.
- W2805528027 cites W4362213396 @default.
- W2805528027 doi "https://doi.org/10.1016/j.icarus.2018.06.001" @default.
- W2805528027 hasPublicationYear "2018" @default.
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